Alkane Resources LtdASX: ALK

Alkane Advances Near-Mine Kendal Deposit with High Grade Antimony-Gold Intercepts at Costerfield

· Issued by Alkane Resources Ltd via GlobeNewswire

PERTH, Australia, Feb. 24, 2026 (GLOBE NEWSWIRE) -- Alkane Resources Limited (ASX: ALK; TSX: ALK; OTCQX: ALKRY) (‘Alkane’ or ‘the Company’) is pleased to announce the latest exploration results for the extension and infill drilling of the Kendal deposit adjoining the currently mined Youle deposit at its Costerfield Operation in central Victoria, Australia.

Program Summary

  • The Kendal system is the antimony-rich, up-dip continuation of the high-grade Youle and Shepherd deposits, where mining is currently underway at Costerfield.

  • Infill and extension drilling over the past year has significantly extended the known size of the vein system, both offset from and adjacent to historic mine workings. Whilst historic mining has been undertaken in the area, this latest drilling has revealed significant veining that was undiscovered when the mine was active between 1861 and 1939.

  • The Kendal veins contain areas of very high gold and antimony grade that have historically correlated with higher production rates.

  • Development to access the newly extended Kendal system began in late 2025 and is ongoing as extension drilling continues.

  • An animation summarising these results will be available at alkres.com

Kendal Assay Highlights

  • From the 501 vein to the south and immediately above Youle:

    • 132.2 g/t gold and 19.8 % antimony over 1.94m (ETW 1.04m) in PD222

    • 25.3 g/t gold and 42.8 % antimony over 1.71m (ETW 0.97m) in PD220

    • 13.5 g/t gold and 22.1% antimony over 2.67m (ETW 1.24m) in AG023

    • 25.4 g/t gold and 8.3 % antimony over 1.28m (ETW 1.12m) in BC437

    • 34.1 g/t gold and 12.9 % antimony over 0.76m (ETW 0.69m) in BC112A

  • From the 520 vein spanning greater than 500m in strike and locally 200m in height.

    • 267.5 g/t gold and 5.6 % antimony over 2.3 m (ETW 1.22m) in BC464

    • 143.7 g/t gold and 10.8 % antimony over 1.35 m (ETW 1.06m) in BC463

    • 18.2 g/t gold and 11.9 % antimony over 2.44 m (ETW 1.92m) in BC466A

Alkane Managing Director & CEO, Nic Earner, said: “The drilling results obtained from the Kendal deposit over the past year demonstrate the large potential remaining for significant high-grade mineralisation at shallow levels near to the Costerfield mine. Accessing and mining the newly defined mineralisation is a top priority for the Costerfield team and should provide the processing plant with an additional source of high-grade gold and antimony ore for some time to come.” 

Costerfield Deposit

Alkane Resources Ltd 100%

The Costerfield antimony-gold deposit was discovered in 1861. Antimony had already been identified in the district as early as 1853, as prospectors attracted to the McIvor (Heathcote) alluvial gold rush began to explore the surrounding hills for the primary deposits. Several lodes along a 3km corridor were rapidly opened up, the bulk of historical production coming from leases at the northern end of the field; the Costerfield (Main), Bombay and Minerva mines. Production from these mines primarily took place in two phases, between 1861-1883 and 1903-1924, and a short-lived attempt at redeveloping the mine occurred between 1933-1939.

Modern mining has been continuous since 2006, when Australian Gold Development (AGD) commenced underground operations at Augusta, at the southern end of the field. AGD’s Costerfield operation was purchased by Mandalay Resources in 2010, and extraction of the vertically continuous vein system has progressively moved north beneath the Costerfield, Minerva and Bombay group of mines, where the high-grade Youle and Shepherd lodes were discovered.

Mandalay Resources merged with Alkane Resources in 2025.

As mining of the underlying vein systems has progressed, it has been recognised that significant amounts of untested mineralisation remain at the level of the historic mines (within 300m of surface) both laterally and within the footprint of the workings. This is primarily due to the structural complexity of the ore system, which consists in places of sheeted vein swarms that can be difficult to interpret along strike without modern methods, including close-spaced drilling that was unavailable to the historic miners.

Regional map of the Costerfield Project in GDA grid showing Alkane tenements and the main corridors of mineralisation identified.

Figure 1. Regional map of the Costerfield Project in GDA grid showing Alkane tenements and the main corridors of mineralisation identified.

Deposit Geology and the Kendal System

The Kendal deposit (and the Costerfield mine) is located on the hinge and western flank of the north-striking Costerfield Anticline which forms the culmination of the Costerfield Dome. The Costerfield Anticline is asymmetrical with a steeply dipping eastern limb, and a gentle dip to the western limb. Numerous smaller scale parasitic folds and warps occupy the broad hinge zone, which often exhibit a weak axial cleavage or parting fabric in the host siltstone. It is this fabric which appears to be the dominant structural host or control for the Kendal veins.

Numerous bedding parallel faults, often containing early-generation laminated quartz veins bisect the system and act as a significant control on grade. Individual veins appear to be offset to the west with depth across these faults, although vein development clearly post-dates fault activity and often can be seen to run along the shallow-dipping faults in a healed manner. Down-dip, the Kendal mineralisation encounters a major west-dipping thrust fault and becomes Youle Lode, which persists downward until the thrust fault begins to shallow, at which point mineralisation breaks back out into a vertical vein system mirroring Kendal, called Shepherd. The Kendal system does not appear to persist into the eastern limb of the greater Costerfield Anticline, which is consistent with other vertical vein systems at Costerfield, potentially due to the lack of cleavage development and small angle between bedding and veining.

Geological cross section of the Costerfield gold-antimony vein system at mine northing 7200N, showing the Kendal vein system’s position in the Costerfield Anticline and its relationship with the below Youle and Shepherd veins which are currently mined.

Figure 2. Geological cross section of the Costerfield gold-antimony vein system at mine northing 7200N, showing the Kendal vein system’s position in the Costerfield Anticline and its relationship with the below Youle and Shepherd veins which are currently mined.

2025 Drilling Program

When the upper portion of Youle Lode was first accessed in 2018 by Mandalay Resources, it was confirmed that the lode system was upwardly continuous, bifurcating and steepening over subhorizontal faulting to form the Kendal system. Over the period of mining, occasional diamond drill holes were placed through Kendal and the adjacent historic mines, which gradually built confidence that a significant amount of mineralisation still existed above the modern mining level. In September 2024, Mandalay Resources issued a TSX announcement, describing the first portion of the Kendal system (the 580 Vein) to be thoroughly tested with modern drilling. The drilling described in this update builds on that work and has tested along the length of the three main historic mines. The bulk of remaining mineralisation identified to date is located adjacent to the Minerva and Costerfield mines, although continuity of the system is demonstrated all the way through to the Bombay mine in the south.

Significant amounts of historical drilling have tested the near-surface portion of the Kendal system, including a campaign of RC percussion drilling conducted by Australian Gold Development in 1995-1996. These historic intercepts have not been verified or validated by Alkane, and their positions are displayed in the release figures due to their relevance to the Kendal target area at height and are indicatory only as support to the geological interpretation.

Drilling Results

With the drill information to date in hand, a total of 25 individual veins have been delineated by Alkane through the Kendal system, building on historical modelling with the inclusion of this program’s drilling data, providing linking intercepts between the three historical mines, and significant extension for some. The Kendal veins extend over a strike of 600m, and some individual veins can be traced for most of this length, for example the 520 vein, which has been interpreted over a length of 500m, with up to 200m of vertical extent. The width of the Kendal system averages around 70m for much of its strike.

The antimony content of the Kendal system, as tested in the program, is significantly higher than that of the Shepherd system, which is a main source of ore for the Costerfield operation, and also demonstrates very high gold content (refer to Appendix 1 for a complete list of significant intercepts from the current drill program).

Many exceptional intercepts were achieved during the program and integrated into the Costerfield geological model. Below are some highlights in addition to those stated above:

  • From the 501 vein:

    • 29.6g/t gold and 50.5% antimony over 0.72m (ETW 0.26m) in PD232

    • 40.6g/t gold and 40.4% antimony over 0.4m (ETW 0.26m) in BC308

    • 30.1g/t gold and 13.4% antimony over 0.67m (ETW 0.55m) in BC438

    • 25g/t gold and 28.1% antimony over 0.67m (ETW 0.36m) in BC328

    • 50g/t gold and 48.3% antimony over 0.21m (ETW 0.2m) in KD529

    • 5.3g/t gold and 5.3% antimony over 1.83m (ETW 1.78m) in KD698

  • From the 519 vein:

    • 52.3g/t gold and 43.1% antimony over 0.34m (ETW 0.29m) in BC468

    • 138g/t gold and 7.7% antimony over 0.27m (ETW 0.21m) in BC143

  • From the 523 vein:

    • 39.4g/t gold and 7.5% antimony over 0.85m (ETW 0.68m) in BC438

    • 261g/t gold and 32.5% antimony over 0.15m (ETW 0.09m) in BC416

  • From the 545 vein:

    • 18.1g/t gold and 12.9% antimony over 1.97m (ETW 1.45m) in BC453

    • 84.4g/t gold and 35.2% antimony over 0.41m (ETW 0.3m) in BC470

  • From the 587 vein:

    • 7.5g/t gold and 5.9% antimony over 2.45m (ETW 1.93m) in BC311

  • From the 590 vein:

    • 13.6g/t gold and 16.4% antimony over 2.22m (ETW 1.37m) in BC418

  • From the 595 vein:

    • 42.2g/t gold and 35.9% antimony over 0.45m (ETW 0.3m) in BC477

    • 41.2g/t gold and 41.8% antimony over 0.32m (ETW 0.23m) in BC465

The 501 vein, which is near modern infrastructure and has recently been accessed for mining, hosts many of the recent (and earlier, unreported) standout intercepts. In addition to the above, several other highly promising intersections were recorded adjacent to the modelled veins:

  • 275g/t gold and 0.1% antimony over 0.49m (ETW 0.4m) in BC125

  • 187g/t gold and 37.8% antimony over 0.35m (ETW 0.32m) in BC313

  • 54.2g/t gold and 50.8% antimony over 0.55m (ETW 0.44m) in BC311

  • 165g/t gold and 34.8% antimony over 0.27m (ETW 0.24m) in BC312

It is anticipated that these intercepts will be integrated into the existing geological model as future drilling adds additional context.

Costerfield / Kendal area plan view with major Kendal vein best fit traces displayed (green), cross section positions (yellow lines), 2025 drill traces and >10g/t AuEq intercepts labelled. Historic Kendal intercept positions are shown as faded circle.

Figure 3. Costerfield / Kendal area plan view with major Kendal vein best fit traces displayed (green), cross section positions (yellow lines), 2025 drill traces and >10g/t AuEq intercepts labelled. Historic Kendal intercept positions are shown as faded circle.

Long Section of the Kendal 501 Vein with high grade assays highlighted. The lower portion of the 501 vein has already been accessed by Alkane, and diluted face grades are shown alongside drilling intercepts.

Figure 4. Long Section of the Kendal 501 Vein with high grade assays highlighted. The lower portion of the 501 vein has already been accessed by Alkane, and diluted face grades are shown alongside drilling intercepts.

Long Section of the Kendal 520 Vein with high grade 2025 assays highlighted. The section shows the strong continuity of the Kendal system outside of the historically mined sections, both vertically and along strike.

Figure 5. Long Section of the Kendal 520 Vein with high grade 2025 assays highlighted. The section shows the strong continuity of the Kendal system outside of the historically mined sections, both vertically and along strike.

The veins are dominantly single-generation, typically consisting of quartz and carbonate, grading to massive stibnite towards the centre line of the veins. Gold can be coarse and present in any part of the vein, and “rusty” gold is often noted, colloform free gold left after the chemical breakdown of the mineral aurostibite, which is common at Costerfield. The veins are surrounded by a narrow (>2m) wallrock sulphide alteration of pyrite and arsenopyrite.

Drill core photos from BC418 (590 Vein) showing the nature of veining with individual assay grades of the samples. Composited interval graded 13.6g/t gold and 16.4% antimony over 2.22m (ETW 1.37m).

Figure 6. Drill core photos from BC418 (590 Vein) showing the nature of veining with individual assay grades of the samples. Composited interval graded 13.6g/t gold and 16.4% antimony over 2.22m (ETW 1.37m).

Photo of drill core from BC463 (520 Vein) showing the sheeted nature of the ore veins. Note the oxidised interval adjacent to the intercept signifies an historical stope adjacent to the in situ high-grade veins. Composited interval graded 143.7g/t gold and 10.8% antimony over 1.35m (ETW 1.06m).

Figure 7. Photo of drill core from BC463 (520 Vein) showing the sheeted nature of the ore veins. Note the oxidised interval adjacent to the intercept signifies an historical stope adjacent to the in situ high-grade veins. Composited interval graded 143.7g/t gold and 10.8% antimony over 1.35m (ETW 1.06m).

Cross section looking north at mine northing 7120N showing Kendal veins in cross section and drill intercepts between 7000N and 7135N. 2025 drill intersections grading over 10g/t AuEq when diluted to 1.8m are labelled. The historic Costerfield Main shaft and workings can be seen centred at 15,500E, and the modern Alkane development offset to the west and depth. Note the average depth of the Kendal mineralisation ascends to the north with the plunge of the anticline.

Figure 8. Cross section looking north at mine northing 7120N showing Kendal veins in cross section and drill intercepts between 7000N and 7135N. 2025 drill intersections grading over 10g/t AuEq when diluted to 1.8m are labelled. The historic Costerfield Main shaft and workings can be seen centred at 15,500E, and the modern Alkane development offset to the west and depth. Note the average depth of the Kendal mineralisation ascends to the north with the plunge of the anticline.

Cross section looking north at mine northing 6780N, showing Kendal veins in cross section and drill intercepts between 6750N and 6825N. 2025 drill intersections grading over 10g/t AuEq when diluted to 1.8m are labelled. This northing passes through the old central Minerva mine and shows the sheeted nature of the east-dipping Costerfield, Minerva and Bombay (540,541 and 542) lodes, in contrast to the northern end of the system where the Costerfield lode is the most significant east-dipping vein.

Figure 9. Cross section looking north at mine northing 6780N, showing Kendal veins in cross section and drill intercepts between 6750N and 6825N. 2025 drill intersections grading over 10g/t AuEq when diluted to 1.8m are labelled. This northing passes through the old central Minerva mine and shows the sheeted nature of the east-dipping Costerfield, Minerva and Bombay (540,541 and 542) lodes, in contrast to the northern end of the system where the Costerfield lode is the most significant east-dipping vein.

Future Plans

Geological modelling and interpretation of results are ongoing, subject to reporting a mineral resource in respect of the Kendal system, the Company intends to work towards integrating those mineral resources into the Costerfield resource and life-of-mine plan in the near future. Early confidence in the southern portions of the tested veins led to the internal decision to begin access development from existing infrastructure late in 2025. Further drilling of the Kendal system is warranted, including on the underexplored Costerfield Main reef to the east of the historic mine. Currently, near mine drilling is focused on the south of the field, where the recently discovered Brunswick South deposit is being drilled alongside extensions to the Cuffley deposit. Drilling at Kendal is expected to resume in 2026.

This document has been authorised for release to the market by Nic Earner, Managing Director and CEO.

ABOUT ALKANE ‐ www.alkres.com ‐ ASX:ALK | TSX: ALK | OTCQX: ALKRY

Alkane (ASX:ALK; TSX:ALK; OTCQX:ALKRY) is an Australia-based gold and antimony producer with a portfolio of three operating mines across Australia and Sweden. The Company has a strong balance sheet and is positioned for further growth.

Alkane’s wholly owned producing assets are the Tomingley open pit and underground gold mine southwest of Dubbo in Central West New South Wales, the Costerfield gold and antimony underground mining operation northeast of Heathcote in Central Victoria, and the Björkdal underground gold mine northwest of Skellefteå in Sweden (approximately 750 km north of Stockholm). Ongoing near-mine regional exploration continues to grow resources at all three operations.

Alkane also owns the very large gold-copper porphyry Boda-Kaiser Project in Central West New South Wales and has outlined an economic development pathway in a Scoping Study. The Company has ongoing exploration within the surrounding Northern Molong Porphyry Project and is confident of further enhancing eastern Australia’s reputation as a significant gold, copper and antimony production region.

Alkane Resources Limited

Competent Persons Statement

As an Australian Company with securities listed on the Australian Securities Exchange (ASX), Alkane is subject to Australian disclosure requirements and standards, including the requirements of the Corporations Act 2001 and the ASX. Investors should note that it is a requirement of the ASX Listing Rules that the reporting of ore reserves and mineral resources in Australia is in accordance with the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (the JORC Code) and that Alkane's ore reserve and mineral resource estimates and reporting comply with the JORC Code.

Alkane is also subject to certain Canadian disclosure requirements and standards as a result of its secondary listing on the Toronto Stock Exchange (TSX), including the requirements of National Instrument 43-101 – Standards of Disclosure for Mineral Projects (NI 43-101). Investors should note that it is a requirement of Canadian securities law that the reporting of mineral reserves and mineral resources in Canada and the disclosure of scientific and technical information concerning a mineral project on a property material to Alkane comply with NI 43-101.

Unless otherwise advised above, or in the relevant ASX announcements referenced, the information in this announcement that relates to exploration results, mineral resources and ore reserves is based on, and fairly represents, information compiled by Mr Chris Davis, who is a Member of the Australasian Institute of Mining and Metallurgy and a full-time employee of Alkane Resources Limited. Mr Davis has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity that is being undertaken to qualify as a Competent Person as defined in the JORC Code and as a Qualified Person under NI 43-101. Mr Davis consents to the inclusion in this announcement of the matters based on his information in the form and context in which they appear. The information in this announcement that relates to previously reported exploration results, mineral resources and ore reserves is extracted from the Company’s ASX announcements noted in the text of the announcement and available to view on the Company’s website. The Company confirms that it is not aware of any new information or data that materially affects the information included in the original announcements and that, in the case of estimates of mineral resources or ore reserves, that all material assumptions and technical parameters underpinning the estimates in the relevant market announcement continue to apply and have not materially changed. The Company confirms that the form and context in which the Competent Person’s findings are presented have not been materially modified from the original market announcement.

Technical Reports released to the TSX or for TSX Market

The NI 43-101 compliant technical report titled ‘NI 43-101 Technical Report, Costerfield Operation, Victoria, Australia’ and dated 28 March 2025, with an effective date of 31 December 2024 supports the information contained herein and is available on the ASX and under Alkane’s profile on SEDAR+ at www.sedarplus.ca.

Reference should be made to the full text of the foregoing technical report for the assumptions, qualifications and limitations relating to the Mineral Resource Estimates and Ore Reserves contained therein and herein. All material assumptions and technical parameters underpinning the estimates in the technical reports continue to apply and have not materially changed.

Cautionary Note Regarding Forward-Looking Information and Statements

This announcement contains certain forward-looking information and forward-looking statements within the meaning of applicable securities legislation and may include future-oriented financial information or financial outlook information (collectively Forward-Looking Information). Actual results and outcomes may vary materially from the amounts set out in any Forward-Looking Information. As well, Forward-Looking Information may relate to: future outlook and anticipated events; expectations regarding exploration potential; production capabilities and future financial or operating performance, including AISC, investment returns, margins and share price performance; production and cost guidance and the timing thereof; issuing updated resources and reserves estimate and the timing thereof; the potential of Alkane to meet industry targets, public profile and expectations; and future plans, projections, objectives, estimates and forecasts and the timing related thereto.

Forward-Looking Information is generally identified by the use of words like "will", "create", "enhance", "improve", "potential", "expect", "upside", "growth" and similar expressions and phrases or statements that certain actions, events or results "may", "could", or "should", or the negative connotation of such terms, are intended to identify Forward-Looking Information.

Although Alkane believes that the expectations reflected in the Forward-Looking Information are reasonable, undue reliance should not be placed on Forward-Looking Information since no assurance can be provided that such expectations will prove to be correct. Forward-Looking Information is based on information available at the time those statements are made and/or good faith belief of the officers and directors of Alkane as of that time with respect to future events and are subject to risks and uncertainties that could cause actual results to differ materially from those expressed in or suggested by the Forward-Looking Information. Forward-Looking Information involves numerous risks and uncertainties. Such factors include, without limitation: risks relating to changes in the gold and antimony price.

Forward-Looking Information is designed to help readers understand Alkane’s views as of that time with respect to future events and speak only as of the date they are made. Except as required by applicable law, Alkane assumes no obligation to update or to publicly announce the results of any change to any forward-looking statement contained or incorporated by reference herein to reflect actual results, future events or developments, changes in assumptions or changes in other factors affecting the Forward-looking Information. If Alkane updates any one or more forward-looking statements, no inference should be drawn that the company will make additional updates with respect to those or other Forward-looking Information. All Forward-Looking Information contained in this announcement is expressly qualified in its entirety by this cautionary statement.

Disclaimer

Alkane has prepared this announcement based on information available to it. No representation or warranty, express or implied, is made as to the fairness, accuracy, completeness or correctness of the information, opinions or conclusions contained in this announcement. To the maximum extent permitted by law, none of Alkane, its directors, officers, employees, associates, advisers and agents, nor any other person accepts any liability, including, without limitation, any liability arising from fault or negligence on the part of any of them or any other person, for any loss arising from the use of this announcement or its contents or otherwise arising in connection with it.

This announcement is not an offer, invitation, solicitation, or other recommendation with respect to the subscription for, purchase or sale of any security, and neither this announcement nor anything in it shall form the basis of any contract or commitment whatsoever.

APPENDIX 1 – Tabulated Drilling Results

Significant intercepts from the Kendal drilling program at Costerfield

Drill Hole ID

From (m)

To (m)

Interval (m)

Estimated True Width (m)

Gold Grade (g/t)

Antimony Grade (%)

Gold-equiv. grade diluted to 1.8 m (g/t)

Interpreted Vein

AG023

68.05

70.72

2.67

1.24

13.5

22.1

45.7

501

BC001

279.14

279.62

0.48

0.38

0.6

0

0.1

501

BC018

224.51

224.68

0.17

0.1

0.6

0

0

501

BC098

210.03

210.12

0.09

0.07

1.6

1

0.2

501

BC112A

105.13

105.89

0.76

0.69

34.1

12.9

24.7

501

BC113

117.96

118.87

0.91

0.75

2.7

1.7

2.9

501

BC114

131.75

132.85

1.1

0.8

3.2

2

3.6

501

BC122

228.01

228.19

0.18

0.14

1.2

0

0.1

501

BC125

42.11

42.55

0.44

0.38

1.6

10.9

5.8

501

BC126

38.92

39.14

0.22

0.2

1.1

8.2

2.3

501

BC307

68.61

68.99

0.38

0.22

39

14.3

9.1

501

BC308

51.96

52.36

0.4

0.26

40.6

40.4

19.7

501

BC311

55.44

55.7

0.26

0.21

18.6

6.5

3.9

501

BC312

32.25

32.35

0.1

0.08

1.2

0

0.1

501

BC313

32.85

32.95

0.1

0.09

1.4

0

0.1

501

BC314

78.97

81.35

2.38

1.21

0.7

1

2.1

501

BC325

62.61

62.73

0.12

0.07

52.3

13.2

3.4

501

BC326

66.16

66.28

0.12

0.07

9

6.8

1

501

BC328

78.34

79.01

0.67

0.36

25

28.1

18.6

501

BC353A

90.85

91

0.15

0.14

1.9

0.9

0.3

501

BC354

154.61

154.81

0.2

0.13

0.8

5.3

1

501

BC358

139.74

139.97

0.23

0.16

5.8

16.6

3.9

501

BC359

65.07

65.35

0.28

0.17

19.3

20.5

6.4

501

BC360

42.44

42.63

0.19

0.13

31.2

0.2

2.3

501

BC361

27.21

28.47

1.26

1.16

3.4

1.6

4.6

501

BC409

120.53

120.71

0.18

0.13

1.1

0.2

0.1

501

BC414A

97.9

98.32

0.42

0.29

6.2

14.9

6.6

501

BC415

103.99

104.45

0.46

0.29

0.4

0

0.1

501

BC416

113.06

114.48

1.42

0.81

0.2

0.7

0.8

501

BC417

147.13

147.3

0.17

0.09

2.4

5

0.7

501

BC437

108.4

109.68

1.28

1.12

25.4

8.3

28.1

501

BC438

114.11

114.78

0.67

0.55

30.1

13.4

19

501

BC439

125.92

126.69

0.77

0.58

1.2

2.3

2.1

501

BC440

115.33

116.69

1.36

1.09

0.7

2.5

4

501

BC441A

127.9

128

0.1

0.07

5.4

20.9

2.3

501

BC442

147.53

147.69

0.16

0.1

151

8.6

9.6

501

BC443

161.71

162.03

0.32

0.18

7.9

11.9

3.6

501

BC444

194.83

197.24

2.41

1.14

1.1

0.9

2

501

BC451

117.73

119.17

1.44

1.16

1.8

2.2

4.6

501

BC461

146.95

147.28

0.33

0.2

18.2

10.2

4.8

501

BC462

114.52

116.1

1.58

1.31

1.4

2.9

6.1

501

BC463

124.43

124.59

0.16

0.12

1.1

5.2

0.9

501

BC468

134.91

135.04

0.13

0.1

0.9

3.7

0.5

501

KD529

71.6

71.81

0.21

0.2

50

48.3

18.6

501

KD530

74.5

74.65

0.15

0.14

2.7

6.3

1.4

501

KD553

35

35.1

0.1

0.09

23.7

3.1

1.5

501

KD556

44.13

44.42

0.29

0.25

24.8

17.1

9.1

501

KD557

51.25

52.3

1.05

0.85

0.1

2

2.2

501

KD576

86

86.13

0.13

0.07

3.7

14.6

1.4

501

KD580

18.7

19

0.3

0.24

0.6

8.1

2.6

501

KD588

16.27

16.6

0.33

0.31

20.5

9.2

7.3

501

KD682

110.08

111.2

1.12

0.85

5.1

1.7

4.3

501

KD684

135

135.16

0.16

0.1

18.7

11.1

2.6

501

KD688

28.4

30.01

1.61

1.2

4.7

1.3

5.2

501

KD696

100.47

101.1

0.63

0.57

5.1

4.6

5.1

501

KD698

102.51

104.34

1.83

1.78

5.3

5.3

17.7

501

MA005

218.31

218.41

0.1

0.07

3.3

5

0.6

501

PD144

38.48

38.61

0.13

0.11

99.9

5.3

7.2

501

PD152

9.41

9.53

0.12

0.1

0.2

11.5

1.6

501

PD153

17.4

20.66

3.26

1.24

0.7

1.2

2.4

501

PD220

13.91

15.62

1.71

0.97

25.3

42.8

68.9

501

PD221A

18.33

21.7

3.37

1.48

2.5

1.3

4.6

501

PD221AB

44.75

46.03

1.28

0.71

2

1.4

2.1

501

PD222

15.01

16.95

1.94

1.04

132.2

19.8

103.3

501

PD224

7.48

7.77

0.29

0.2

1.6

8.8

2.5

501

PD232

8.91

9.63

0.72

0.26

29.6

50.5

21.8

501

PD254

75.01

75.18

0.17

0.1

32.6

16.4

3.8

501

PD255

56.58

56.93

0.35

0.26

0.2

3.8

1.3

501

PD256

43.21

43.46

0.25

0.23

0.1

0

0

501

PD257

62.64

62.83

0.19

0.12

12.4

41.7

7.4

501

BC308

109.24

109.36

0.12

0.08

5.8

7.7

1.1

517

BC437

135.17

135.38

0.21

0.17

2

28

6.5

517

BC441

182.86

183.21

0.35

0.27

30.4

17.8

11.1

517

BC462

147.52

147.92

0.4

0.36

0.2

0.4

0.2

517

BC311

72

72.11

0.11

0.05

1

0

0

518

BC360

80.06

83.86

3.8

1.45

0.5

0.7

1.7

518

BC437

128.36

128.46

0.1

0.06

1.2

0

0

518

BC008

228.45

229.95

1.5

1.17

2.3

3

6.1

519

BC113

138.72

138.86

0.14

0.13

51.9

15.8

6.4

519

BC143

213.05

213.32

0.27

0.21

138

7.7

17.9

519

BC308

94.88

97.13

2.25

1.66

1.7

2.4

7

519

BC314

111.98

113.17

1.19

0.73

0.8

1.5

1.8

519

BC354

191.13

191.94

0.81

0.58

1.6

1

1.3

519

BC434

170.88

170.98

0.1

0.07

1.8

0.1

0.1

519

BC442

182.14

182.71

0.57

0.35

0.7

1.9

1

519

BC448

140.57

140.72

0.15

0.13

0.4

37.2

6.6

519

BC451

139.62

141.26

1.64

1.49

0.4

0.9

2.1

519

BC456

166.93

167.63

0.7

0.47

0.1

0

0

519

BC458

218.61

219.61

1

0.51

0.1

0.5

0.4

519

BC461

177.15

177.59

0.44

0.26

1

5.6

2.1

519

BC465

185.72

186.2

0.48

0.31

10.1

1

2.2

519

BC466A

159.27

159.43

0.16

0.13

1.1

2

0.5

519

BC468

159.87

160.21

0.34

0.29

52.3

43.1

24.7

519

BC470

177.1

177.25

0.15

0.07

4.1

1.2

0.3

519

BC477

197.93

198.04

0.11

0.06

13.4

14.3

1.7

519

BC482

237.04

238.53

1.49

0.56

12.7

2.5

5.9

519

MA002

156.37

156.92

0.55

0.44

0.2

0.7

0.5

519

AG247W1

267.54

267.87

0.33

0.21

18.3

14.9

6.2

520

BC003

81.37

83.46

2.09

1.35

7.9

1.1

8

520

BC003A

81.82

83.54

1.72

1.14

2.1

1.6

3.7

520

BC008

251.5

252.65

1.15

0.87

2.6

1.1

2.5

520

BC010

290.9

291

0.1

0.07

0.2

0

0

520

BC012

29.78

29.92

0.14

0.02

7.2

0.3

0.1

520

BC108

186.63

186.81

0.18

0.12

3.5

4.4

0.9

520

BC112A

110.87

111.74

0.87

0.76

2.6

2.9

4.1

520

BC114

136.17

136.29

0.12

0.09

0.6

1.2

0.2

520

BC128

225.36

225.52

0.16

0.09

40.4

7.2

2.9

520

BC307

76.96

77.11

0.15

0.11

13.3

3.7

1.4

520

BC308

69.73

71.37

1.64

1.12

3

3.8

7.5

520

BC311

62.38

63.28

0.9

0.7

10.7

8.1

11.7

520

BC314

85.05

85.28

0.23

0.16

24.3

16.1

5.4

520

BC325

74.22

74.53

0.31

0.22

0.1

0

0

520

BC328

90.16

90.29

0.13

0.07

0.9

0.8

0.1

520

BC354

170.39

170.51

0.12

0.09

2.8

2.6

0.4

520

BC359

81.03

81.16

0.13

0.08

5.1

0.6

0.3

520

BC360

70.12

70.7

0.58

0.43

0.6

2

1.3

520

BC404

243.25

243.63

0.38

0.21

0.4

0

0

520

BC414A

99

99.63

0.63

0.43

0

0.5

0.3

520

BC415

114.02

114.4

0.38

0.24

0.3

7.1

2.3

520

BC416

122.25

123.65

1.4

0.83

1.1

2

2.7

520

BC417

155.79

156.76

0.97

0.46

10.9

6.8

7

520

BC418

191.02

191.96

0.94

0.6

3.2

6.2

6

520

BC419

217.7

217.89

0.19

0.11

3.6

1.1

0.4

520

BC424

268.45

268.61

0.16

0.08

2

8.1

0.9

520

BC426

181.41

181.72

0.31

0.21

0.1

0

0

520

BC430

192.67

193.45

0.78

0.49

5.4

3.8

3.9

520

BC437

114.58

114.7

0.12

0.1

3.9

6.4

1.1

520

BC438

119

119.33

0.33

0.26

13

10.8

5.7

520

BC439

127.8

128.46

0.66

0.52

15.6

2.5

6.3

520

BC440

120.3

120.48

0.18

0.14

14.9

8.8

2.8

520

BC442

156.12

156.22

0.1

0.07

1.8

2.1

0.3

520

BC443

176

176.47

0.47

0.3

0.6

0.5

0.3

520

BC448

124.13

125.05

0.92

0.77

7.3

5.7

8.9

520

BC455

143.55

145.72

2.17

1.5

3

3.6

9.6

520

BC456

155.57

156.74

1.17

0.81

1

2.7

3.4

520

BC457

207.73

208.28

0.55

0.28

9.4

4.2

3

520

BC458

188.81

189.61

0.8

0.47

0.6

1.6

1.2

520

BC459

203.68

203.83

0.15

0.08

7.8

8.4

1.3

520

BC460

209.29

209.39

0.1

0.05

1.1

1.8

0.2

520

BC461

154.93

156.54

1.61

1.07

0.9

2.4

4

520

BC462

119.47

119.6

0.13

0.11

2

4

0.7

520

BC463

133

134.35

1.35

1.06

143.7

10.8

100.1

520

BC464

206.2

208.5

2.3

1.22

267.5

5.6

190.6

520

BC465

162.35

162.68

0.33

0.23

5.9

0.3

0.8

520

BC466A

131.47

133.91

2.44

1.92

18.2

11.9

46.6

520

BC468

137.85

138.63

0.78

0.6

1.4

1.3

1.5

520

BC476

218.36

219.78

1.42

0.68

0.6

0.9

1.1

520

BC477

172.41

172.58

0.17

0.11

38.1

2.4

2.7

520

MA001

129.09

131.94

2.85

0.12

0.7

1.3

0.2

520

MA004

138.02

138.3

0.28

0.01

6.7

39.3

0.6

520

MA005

206.47

206.73

0.26

0.2

9.1

6.9

2.8

520

PD221A

52.57

52.74

0.17

0.1

14

7.7

1.8

520

PD254

82.9

83.51

0.61

0.34

0.2

0

0

520

PD255

64.38

64.89

0.51

0.38

30.2

5.4

9

520

BC003

79.63

79.74

0.11

0.06

40.7

22.7

3

522

BC003A

77.75

77.9

0.15

0.08

30.3

9.3

2.3

522

BC012

39.13

39.48

0.35

0.3

1

0

0.2

522

BC457

198.29

201.01

2.72

2.07

1.4

1.4

4.8

522

BC464

205.2

206.2

1

0.74

6.8

3.3

6.1

522

BC475

215.4

221.94

6.54

4.5

2.3

1.4

5.6

522

BC113

129.91

130.04

0.13

0.1

12.5

16.4

2.9

523

BC114

140.74

140.85

0.11

0.08

0

1

0.1

523

BC328

93.99

94.49

0.5

0.3

0.5

0.2

0.2

523

BC359

84.1

84.25

0.15

0.1

1.1

1.5

0.3

523

BC416

136.37

136.52

0.15

0.09

261

32.5

17

523

BC438

127.4

128.25

0.85

0.68

39.4

7.5

21.5

523

BC439

132.5

132.63

0.13

0.1

3.5

2

0.4

523

BC440

129.43

129.66

0.23

0.18

18.2

7.1

3.5

523

BC441

146.21

146.31

0.1

0.07

1.1

1.4

0.2

523

BC441A

138.2

138.36

0.16

0.11

1

2.6

0.5

523

BC442

159.69

160.36

0.67

0.38

0.3

1

0.6

523

BC450

133.65

133.86

0.21

0.15

0.2

0.9

0.2

523

BC451

132.03

132.2

0.17

0.13

1.1

0.9

0.2

523

BC466A

146.29

146.44

0.15

0.11

14.3

0.5

1

523

BC468

147.26

147.47

0.21

0.15

1.9

0.5

0.3

523

PD221A

62.38

62.67

0.29

0.17

2.2

3.3

1

523

BC004

88.16

88.25

0.09

0.06

0.3

1

0.1

540

BC005

29.19

29.34

0.15

0.1

1.5

0.1

0.1

540

BC008

198.67

199.72

1.05

0.95

0.5

3.3

4.4

540

BC113

195.67

195.9

0.23

0.23

0.2

0

0

540

BC114

197.74

198.02

0.28

0.26

1.4

1.7

0.8

540

BC142

111.12

116.97

5.85

2.64

2.6

3.3

10.6

540

BC143

301.58

302.28

0.7

0.24

0.4

4.7

1.6

540

BC307

111.26

111.45

0.19

0.18

1.2

1.5

0.5

540

BC308

121.04

121.33

0.29

0.25

0.3

2.1

0.8

540

BC314

138.67

138.78

0.11

0.08

2.1

3.1

0.4

540

BC325

101.33

101.57

0.24

0.23

6.7

9

3.6

540

BC326

107.52

107.92

0.4

0.36

1.1

1.4

0.9

540

BC360

105.85

106.18

0.33

0.3

0.5

2.6

1.1

540

BC418

249.4

249.54

0.14

0.12

10.6

7.1

1.9

540

BC430

240.74

241.79

1.05

0.88

0.7

1.4

1.9

540

BC434

218.48

218.96

0.48

0.46

1.1

8.6

5.5

540

BC443

220.78

221.78

1

0.77

0.6

0.3

0.6

540

BC455

236.48

236.94

0.46

0.38

19.1

17.3

12.9

540

BC456

206.69

207.09

0.4

0.36

0.1

0

0

540

BC468

209

209.34

0.34

0.32

0.3

1.4

0.7

540

BC481

237.47

237.8

0.33

0.27

7.7

11.2

5.2

540

MA001

141.49

141.58

0.09

0.04

3.2

9.8

0.5

540

MA002

171.75

171.83

0.08

0.04

1.2

14.9

0.9

540

TP009

88.35

88.46

0.11

0.05

2.1

8.1

0.5

540

TP018

69.32

69.45

0.13

0.05

1.2

0

0

540

BC457

259.83

260.01

0.18

0.12

2.4

0.1

0.2

541

BC458

255.91

256.07

0.16

0.1

1

1.3

0.2

541

BC464

261.12

261.45

0.33

0.19

12.4

0

1.3

541

AG020

155.55

156.04

0.49

0.43

0.1

0

0

542

BC003

139.7

140.5

0.8

0.39

33.2

2.1

8.4

542

BC142

199.24

199.62

0.38

0.25

12.6

3.1

2.8

542

BC442

256.3

257.2

0.9

0.73

1

0.2

0.6

542

BC456

239.55

239.69

0.14

0.12

3.1

0.9

0.3

542

BC003

112

112.17

0.17

0.12

0.2

0.3

0.1

545

BC129

177.98

178.32

0.34

0.29

0.7

0

0.1

545

BC130

196.74

196.97

0.23

0.18

11.7

38.7

10.2

545

BC143

250.09

250.18

0.09

0.06

0.1

6.7

0.6

545

BC434

173.82

173.97

0.15

0.13

5.7

21.2

4

545

BC445

186.6

186.83

0.23

0.18

2.4

31.4

7.8

545

BC446

179.5

179.89

0.39

0.31

3.9

15

6.8

545

BC447

171.16

171.38

0.22

0.18

2.7

14.3

3.7

545

BC450

162.88

162.99

0.11

0.09

2.7

7.8

1.1

545

BC452

189.72

189.88

0.16

0.12

18

22.2

4.8

545

BC453

195.06

197.03

1.97

1.45

18.1

12.9

39.4

545

BC454

185.8

185.98

0.18

0.14

1.7

9.9

2

545

BC469

205.09

205.19

0.1

0.07

2.6

16.5

1.6

545

BC470

203.53

203.94

0.41

0.3

84.4

35.2

28.4

545

BC481

216.15

216.7

0.55

0.37

9.8

12.9

8.3

545

BC482

263.75

263.91

0.16

0.1

1.3

5.6

0.8

545

BC004

43.36

44.1

0.74

0.59

0

0

0

585

BC009

214.76

214.86

0.1

0.08

0.6

0

0

585

BC010

241.06

241.33

0.27

0.19

21.1

12.5

5.3

585

BC108

116.02

116.18

0.16

0.11

13.5

7.8

1.9

585

BC113

106.12

106.59

0.47

0.37

0

0

0

585

BC122

209.17

209.5

0.33

0.26

1.1

10.7

3.8

585

BC128

136.47

136.67

0.2

0.12

6

11.8

2.3

585

BC129

108.72

108.88

0.16

0.12

2.1

0.8

0.3

585

BC143

170.44

170.62

0.19

0.11

1.7

0

0.1

585

BC397

175.59

175.93

0.34

0.16

2.1

0

0.2

585

BC398

124.25

124.42

0.17

0.11

38.3

15.6

4.7

585

BC404

148.05

154.16

6.11

3.67

0.4

0

0.5

585

BC406

107.58

108.46

0.88

0.68

14.5

5.1

10.1

585

BC408

133.83

135.15

1.32

0.84

4.3

1.9

4.1

585

BC409

114.12

115.28

1.16

0.84

7.1

3.3

7

585

BC418

118.2

118.32

0.12

0.09

15.4

16.1

2.6

585

BC419

135.76

135.89

0.13

0.08

31

24.3

4.1

585

BC420

185.3

185.59

0.29

0.14

1.9

0

0.2

585

BC421

316.33

316.58

0.25

0.09

68.8

41.7

8.3

585

BC423

147.58

147.75

0.17

0.1

6.6

10.2

1.7

585

BC424

152.61

152.73

0.12

0.07

19.9

0.1

0.7

585

BC425

106.44

107.22

0.78

0.62

4.5

11.1

10.7

585

BC426

115.69

116.73

1.04

0.76

1.4

4.2

4.8

585

BC427

222.68

223.84

1.16

0.52

3.3

5.4

4.7

585

BC428

102.55

102.96

0.41

0.35

0

0.1

0.1

585

BC430

119.75

119.96

0.21

0.14

24.7

32

7.9

585

BC431

133.11

133.35

0.24

0.15

46.7

36.2

11.4

585

BC434

107.81

109.36

1.55

1.19

0.3

1.4

2.4

585

BC437

101

102.68

1.68

1.41

4.4

1.4

6.1

585

BC445

121.14

121.24

0.1

0.07

1.7

1

0.2

585

BC446

112.3

112.78

0.48

0.3

4.5

10.2

4.8

585

BC448

105.31

106.05

0.74

0.56

0.9

3.9

3.1

585

BC449

170.53

170.92

0.39

0.19

10.9

17.7

5.5

585

BC452

126.86

127.79

0.93

0.55

0.5

0

0.2

585

BC453

128.68

129.1

0.42

0.23

0.5

1.6

0.6

585

BC454

111.51

111.64

0.13

0.07

2.5

29.1

2.9

585

BC455

115.93

116.07

0.14

0.08

1.7

0

0.1

585

BC466A

108.1

109.23

1.13

0.78

0.4

0.7

0.8

585

BC467

126.69

127.14

0.45

0.25

0.8

1.1

0.5

585

BC469

135.15

135.69

0.54

0.3

1.9

4.4

2

585

BC482

153

153.16

0.16

0.05

10.7

13.4

1.3

585

KD681

93.52

93.63

0.11

0.09

2.9

17.7

2.4

585

KD683

111.26

111.35

0.09

0.07

1.7

0

0.1

585

KD684

122.2

122.83

0.63

0.43

0.4

0.1

0.1

585

KD696

92.56

93.87

1.31

1.17

3.7

2.8

6.8

585

KD698

99.04

99.73

0.69

0.62

4

4.1

4.7

585

KD700

134.03

134.18

0.15

0.11

1.9

0

0.1

585

KD701

104.53

104.63

0.1

0.09

1.8

0

0.1

585

KD702

124.85

125.68

0.83

0.63

0.6

0

0.2

585

AG019

273.17

273.26

0.09

0.07

0.3

14.2

1.4

587

BC003

49

49.14

0.14

0.11

0.6

10.5

1.5

587

BC004

50

50.2

0.2

0.13

0

0

0

587

BC008

270.07

270.17

0.1

0.07

2

0

0.1

587

BC009

223.79

223.9

0.11

0.07

1.5

0.1

0.1

587

BC010

256.66

257.2

0.54

0.3

0.5

0

0.1

587

BC108

153.36

153.57

0.21

0.13

1.4

19

3.3

587

BC112A

100.49

103.39

2.9

2.53

2

2.8

8.7

587

BC113

113.19

113.33

0.14

0.11

30

11.7

3.6

587

BC114

125.85

125.96

0.11

0.08

2.1

4.2

0.5

587

BC128

154.81

154.98

0.17

0.09

2

0.5

0.2

587

BC129

119.78

119.96

0.18

0.16

3.5

7.4

1.9

587

BC130

141.42

141.58

0.16

0.13

3.4

0.2

0.3

587

BC143

182.52

182.97

0.45

0.27

0.2

9.8

3.5

587

BC307

57.47

57.68

0.21

0.12

0.3

15.4

2.5

587

BC311

49

51.45

2.45

1.93

7.5

5.9

21.7

587

BC314

62.31

62.59

0.28

0.14

5.6

5.8

1.5

587

BC325

58.02

58.15

0.13

0.08

0.5

1.2

0.1

587

BC326

60.41

60.68

0.27

0.15

1.6

0

0.1

587

BC328

68.58

68.75

0.17

0.09

25.8

3.8

1.8

587

BC354

148.93

149.2

0.27

0.17

1

0

0.1

587

BC359

59.82

59.97

0.15

0.09

2.2

2.2

0.4

587

BC404

191.52

192.37

0.85

0.43

5.8

5.8

4.7

587

BC414A

90.03

91.12

1.09

0.74

0.2

0.4

0.5

587

BC416

110.18

111.06

0.88

0.5

1.6

0.7

0.9

587

BC417

133.4

136.21

2.81

1.26

8.4

4.2

12.9

587

BC418

129.58

130

0.42

0.36

0.8

16.3

7.9

587

BC419

159.42

159.59

0.17

0.1

8.3

24.6

3.6

587

BC421

353.35

353.54

0.19

0.05

1.3

10.5

0.7

587

BC423

176.31

178.93

2.62

1.3

0.7

1.2

2.6

587

BC424

200.87

201.03

0.16

0.07

51.4

36.5

5.6

587

BC425

119.08

119.27

0.19

0.17

12.3

6.8

2.7

587

BC426

135.39

135.49

0.1

0.07

2.2

0

0.1

587

BC428

118.12

118.35

0.23

0.22

0.8

3.4

1.1

587

BC430

134.74

134.89

0.15

0.12

31.9

15.2

4.6

587

BC431

152.76

152.86

0.1

0.06

1.3

0

0

587

BC434

123.91

124.01

0.1

0.09

1.5

0

0.1

587

BC437

104.61

107

2.39

2.01

1

2.5

7

587

BC438

109.13

109.27

0.14

0.11

0.3

1.5

0.2

587

BC439

118.24

118.87

0.63

0.47

0.6

0.7

0.6

587

BC440

112.24

113

0.76

0.61

8.8

11.3

12.2

587

BC441

130.85

131.01

0.16

0.11

3.5

0.8

0.3

587

BC441A

124

124.1

0.1

0.07

0.9

0.9

0.1

587

BC442

141.88

141.98

0.1

0.06

1

0

0

587

BC443

156.62

157.33

0.71

0.4

17.6

10.9

9.7

587

BC444

174.57

176.1

1.53

0.73

1.4

3.8

4.2

587

BC445

133.98

134.11

0.13

0.11

0.9

0.9

0.2

587

BC446

130.56

130.83

0.27

0.23

1.8

0.8

0.5

587

BC447

121.27

121.42

0.15

0.11

1.6

6.5

1

587

BC448

107.61

110.85

3.24

2.64

1.1

0.7

2.7

587

BC449

183.73

183.84

0.11

0.07

25.3

1.9

1.2

587

BC450

119.14

119.91

0.77

0.57

3.2

2.9

3.2

587

BC451

112.55

114.29

1.74

1.37

3.2

1.7

5.5

587

BC452

135.89

136.04

0.15

0.12

0.9

2.4

0.5

587

BC453

138.43

138.55

0.12

0.1

17.7

11

2.4

587

BC454

132.68

132.84

0.16

0.11

2.8

12.7

2

587

BC455

117.9

118

0.1

0.07

0.9

0

0

587

BC457

175.76

177.11

1.35

0.68

1.1

0.3

0.7

587

BC458

157.38

157.48

0.1

0.05

1.8

6.1

0.5

587

BC459

166.8

166.9

0.1

0.05

3.3

2

0.2

587

BC460

198

198.19

0.19

0.09

1.3

1

0.2

587

BC461

142.37

144.3

1.93

1.18

3

6.4

12

587

BC462

109.62

109.77

0.15

0.12

0.9

1.3

0.3

587

BC463

117.9

118.89

0.99

0.73

0.1

0.2

0.3

587

BC464

176.4

177.58

1.18

0.57

0.3

0.2

0.2

587

BC465

142.23

142.43

0.2

0.13

1.1

0.3

0.1

587

BC467

134.29

134.61

0.32

0.22

0.5

5.5

1.7

587

BC469

146.83

147.16

0.33

0.26

0.1

5.2

1.8

587

BC477

145.1

145.21

0.11

0.06

4.5

6.3

0.7

587

BC481

153.3

153.6

0.3

0.22

40.6

37.1

15.8

587

BC483

152.13

152.78

0.65

0.38

1

8.7

4.6

587

KD574

51.36

51.49

0.13

0.09

47.2

25.2

5.4

587

KD576

76.69

79.3

2.61

1.31

1.8

0.5

2.3

587

PD221A

38.43

40.03

1.6

0.87

1.4

3.1

4.2

587

PD224

30

30.54

0.54

0.34

0.1

0

0

587

PD254

66.22

66.85

0.63

0.35

1.4

10.1

5

587

PD257

61.17

61.33

0.16

0.1

3.8

5.4

0.9

587

BC009

229.53

229.69

0.16

0.12

1.9

1.2

0.3

589

BC010

274.53

274.74

0.21

0.14

1

0

0.1

589

BC129

140.38

140.55

0.17

0.13

1.4

0

0.1

589

BC419

178.67

179.62

0.95

0.5

1.3

2

1.7

589

BC424

215.16

215.26

0.1

0.04

6.7

7.3

0.6

589

BC425

134.31

134.41

0.1

0.08

1.9

3.8

0.5

589

BC426

147.63

149.62

1.99

1.22

2.4

1.6

4.3

589

BC428

127.75

127.85

0.1

0.08

0.7

2

0.3

589

BC431

178.19

178.69

0.5

0.26

1.1

1.5

0.7

589

BC434

131.86

131.96

0.1

0.08

13.9

19.1

2.7

589

BC449

211.34

211.57

0.23

0.11

39.4

0.4

2.4

589

BC482

185.8

186.1

0.3

0.14

8.8

8.8

2.3

589

BC003

67.71

67.91

0.2

0.14

0.1

0

0

590

BC004

61.27

61.42

0.15

0.13

2.9

15.4

2.8

590

BC009

238.07

238.39

0.32

0.25

0.2

0

0

590

BC128

211.4

211.56

0.16

0.08

5.5

1.6

0.4

590

BC130

157.1

158.81

1.71

1.35

2.2

0.7

3

590

BC143

199.42

202.29

2.87

2.44

0.4

0.7

2.1

590

BC404

213.75

213.92

0.17

0.1

10.2

14.7

2.4

590

BC418

176.09

178.31

2.22

1.37

13.6

16.4

40.2

590

BC424

234.48

234.67

0.19

0.09

6.2

0

0.3

590

BC425

154.25

154.4

0.15

0.11

24.4

21.4

4.6

590

BC426

160.7

161.22

0.52

0.34

16.8

26.1

15

590

BC428

142.39

143.8

1.41

1.09

6.6

4.9

11.1

590

BC430

183.26

185.33

2.07

1.1

2.1

1.6

3.6

590

BC431

203.46

206.01

2.55

1.46

4.5

1.7

7

590

BC445

155.74

155.84

0.1

0.06

3.3

5.3

0.6

590

BC446

143.88

144.05

0.17

0.14

4.3

4.4

1.1

590

BC452

154.17

156.31

2.14

1.57

0.8

1.2

3.2

590

BC453

154.21

154.34

0.13

0.1

6

3.7

0.8

590

BC469

164.7

166.63

1.93

1.35

4.7

3.1

9.2

590

BC420

164.29

164.51

0.22

0.09

7

21.8

3.1

592

BC422

191.4

191.55

0.15

0.05

1.1

0.4

0.1

592

BC427

206.65

206.9

0.25

0.1

7.3

5.4

1.1

592

BC429

245.48

245.67

0.19

0.06

1.2

0

0

592

BC010

285.17

285.37

0.2

0.14

0.7

0

0.1

593

BC425

145.58

145.84

0.26

0.2

24.8

5.8

4.4

593

BC427

289.99

290.3

0.31

0.13

1.5

0.2

0.1

593

BC428

135.43

135.56

0.13

0.11

20.5

24.3

4.8

593

BC430

169.48

169.58

0.1

0.06

2.8

4.6

0.5

593

BC431

193

193.23

0.23

0.14

36.9

10.9

5.1

593

BC434

138.34

138.44

0.1

0.08

3.9

5.5

0.8

593

BC445

150.62

150.8

0.18

0.14

0.7

0.2

0.1

593

BC008

240.7

241.5

0.8

0.65

29.3

2.3

12.6

595

BC314

107.74

108.83

1.09

0.69

0.8

0.5

0.8

595

BC456

161.97

162.2

0.23

0.17

13.5

17.9

5.3

595

BC457

210.5

212.82

2.32

1.4

15.5

2.5

16.6

595

BC458

201.71

202.05

0.34

0.21

40

18.5

9.8

595

BC459

225

225.76

0.76

0.42

1

0.7

0.6

595

BC464

223.31

223.76

0.45

0.25

0.3

0.6

0.2

595

BC465

173.4

173.72

0.32

0.23

41.2

41.8

18.3

595

BC476

237.68

238.19

0.51

0.24

2

1.4

0.7

595

BC477

180.64

181.09

0.45

0.3

42.2

35.9

21.6

595

BC130

172.48

176.05

3.57

2.6

3.3

0.7

4.9

596

BC434

159.97

161.1

1.13

0.9

0.4

0.3

0.6

596

BC445

167.57

169.95

2.38

1.77

2.8

2.8

9.3

596

BC446

156.18

157.36

1.18

0.85

0.3

0.1

0.3

596

BC447

149.17

149.35

0.18

0.14

18.9

4.9

2.3

596

BC454

164.46

164.9

0.44

0.31

27.1

11.5

9.3

596

BC130

168.31

168.92

0.61

0.44

31.8

3.9

10

597

BC453

165.66

166.46

0.8

0.42

2.9

2.1

1.8

597

BC307

52.43

52.61

0.18

0.08

1.5

0.6

0.1

50101

BC308

41.32

41.53

0.21

0.12

0.6

0

0

50101

BC314

57.58

57.74

0.16

0.07

1.3

19.1

1.7

50101

BC325

53.42

53.79

0.37

0.18

0.2

1

0.3

50101

BC326

59.51

59.76

0.25

0.11

1.5

3.9

0.7

50101

BC328

62.83

63.13

0.3

0.15

1.1

0

0.1

50101

BC354

143.1

143.2

0.1

0.06

3.1

2.3

0.3

50101

BC359

51.2

51.35

0.15

0.08

0.8

0

0

50101

BC360

39.51

39.61

0.1

0.06

0.1

0

0

50101

KD530

73.56

73.7

0.14

0.13

0.4

12.4

2.2

50101

KD574

44.45

47.08

2.63

1.84

0.9

1

3.3

50101

KD588

10.9

11.04

0.14

0.13

2.6

12.2

2.3

50101

PD144

34.14

34.53

0.39

0.35

9.1

6.2

4.7

50101

PD254

51.01

51.5

0.49

0.26

0.8

1.4

0.6

50101

PD255

46.17

46.69

0.52

0.36

6.5

1.6

2.1

50101

PD256

37.61

37.71

0.1

0.08

29.3

11.4

2.6

50101

BC008

289.09

289.19

0.1

0.07

0.9

0

0

50102

BC414A

76.91

77.15

0.24

0.14

11.4

16.2

3.9

50102

BC415

91.19

91.39

0.2

0.1

12.7

12.4

2.4

50102

BC416

102.04

102.2

0.16

0.07

3.6

18.8

2

50102

BC442

125.32

125.49

0.17

0.1

30.2

13.2

3.6

50102

BC443

135.85

136.01

0.16

0.09

14.7

15.3

2.6

50102

BC444

147.65

149.25

1.6

0.79

0.6

0.3

0.5

50102

BC461

121.94

122.07

0.13

0.08

4.3

7.3

1

50102

BC463

112.66

112.88

0.22

0.16

14.7

10.1

3.5

50102

KD576

68.72

68.88

0.16

0.06

20.1

10.4

1.6

50102

BC114

110.18

110.29

0.11

0.07

0.9

22.6

2.2

50103

BC414A

67.88

68

0.12

0.05

3.5

7

0.5

50103

BC415

79.8

79.97

0.17

0.07

28

26.5

3.4

50103

BC416

91.48

91.59

0.11

0.04

1.6

0

0

50103

BC439

110.86

111

0.14

0.09

1.7

0.2

0.1

50103

BC440

105.16

105.26

0.1

0.07

7.3

0.2

0.3

50103

BC441

110.76

110.86

0.1

0.07

2

3.3

0.4

50103

BC441A

110.96

111.06

0.1

0.07

2.6

2.7

0.4

50103

BC442

117.17

117.27

0.1

0.06

1.8

0.7

0.1

50103

BC443

126.41

126.56

0.15

0.09

1.9

5.8

0.8

50103

BC444

137.73

138.35

0.62

0.36

1.2

0.8

0.6

50103

BC456

114.72

115.47

0.75

0.43

1.5

0.6

0.7

50103

BC461

114.45

114.55

0.1

0.06

1.4

0

0.1

50103

BC462

104.07

104.17

0.1

0.08

0.1

0.1

0

50103

KD576

48

49

1

0.16

12.9

1.1

1.4

50103

BC003

85.41

85.61

0.2

0.15

3.5

15.6

3.3

Associated

BC112A

99.35

99.53

0.18

0.16

0.2

10.3

2.2

Associated

BC112A

107.16

107.42

0.26

0.24

13.4

1

2.1

Associated

BC114

169.59

169.77

0.18

0.13

9.2

17.1

3.7

Associated

BC114

170.77

170.91

0.14

0.1

19.1

13.6

2.9

Associated

BC114

173.62

173.83

0.21

0.15

122

6.4

11.7

Associated

BC125

37.1

37.21

0.11

0.09

143

8.3

8.1

Associated

BC125

37.21

37.98

0.77

0.62

0.4

5.6

4.7

Associated

BC125

39.31

39.59

0.28

0.23

23.2

0.3

3

Associated

BC125

44.64

45.13

0.49

0.4

275

0.1

60.8

Associated

BC129

156.62

156.83

0.21

0.16

14.8

14.5

4.4

Associated

BC129

158.84

159

0.16

0.12

9.9

8.6

2.1

Associated

BC129

164.9

165.07

0.17

0.13

92.4

39.3

13.6

Associated

BC143

203.94

204.39

0.45

0.28

4.2

4

2.2

Associated

BC143

210.62

211.31

0.69

0.43

3

2.4

2.1

Associated

BC308

91.78

91.89

0.11

0.08

4.6

17.3

2.1

Associated

BC308

93.06

93.17

0.11

0.08

41.5

15.9

3.6

Associated

BC308

99.23

99.43

0.2

0.15

47.7

6.7

5.3

Associated

BC311

0.49

0.72

0.23

0.18

17.5

16.7

5.9

Associated

BC311

2.55

3.5

0.95

0.76

1.1

2

2.5

Associated

BC311

3.5

4.05

0.55

0.44

54.2

50.8

43

Associated

BC312

0.3

0.4

0.1

0.09

7.9

27.7

3.6

Associated

BC312

1.1

1.37

0.27

0.24

165

34.8

32.9

Associated

BC313

0

0.41

0.41

0.38

0.8

7.2

3.8

Associated

BC313

1.2

1.55

0.35

0.32

187

37.8

49.7

Associated

BC314

113.17

113.31

0.14

0.08

59.7

11.8

4

Associated

BC354

131.03

131.3

0.27

0.19

21.2

12

5.3

Associated

BC398

99.64

99.88

0.24

0.14

11.4

24.3

5.3

Associated

BC416

142.73

143.18

0.45

0.29

23.7

1.6

4.5

Associated

BC418

193.51

193.64

0.13

0.09

15.1

19.1

2.9

Associated

BC423

173.98

174.28

0.3

0.16

7.9

10.8

3

Associated

BC426

181.72

182.15

0.43

0.3

28.5

0

4.8

Associated

BC426

182.15

182.5

0.35

0.25

3.3

6.8

2.7

Associated

BC430

189.84

190.1

0.26

0.16

24.8

3.3

2.9

Associated

BC431

208.9

209.08

0.18

0.11

28.8

10.3

3.4

Associated

BC434

150.75

151.2

0.45

0.36

7.6

1.9

2.5

Associated

BC434

170.98

171.8

0.82

0.66

6

0.1

2.3

Associated

BC437

112.24

112.34

0.1

0.09

28.2

12.1

2.8

Associated

BC439

127.05

127.5

0.45

0.35

6.5

2.7

2.5

Associated

BC440

138.41

138.52

0.11

0.09

21.1

10.3

2.3

Associated

BC440

140.15

140.39

0.24

0.19

5.4

11.6

3.6

Associated

BC441

164.3

164.53

0.23

0.15

6.3

9.7

2.5

Associated

BC443

209.09

209.32

0.23

0.12

9.8

14.6

3

Associated

BC446

145.91

146.1

0.19

0.13

86.9

8.8

8

Associated

BC446

149.05

149.57

0.52

0.36

4.4

2.7

2.2

Associated

BC447

49.49

49.79

0.3

0.22

1

13.7

4.1

Associated

BC447

136.48

136.86

0.38

0.28

4.1

5.2

2.6

Associated

BC449

204.82

204.94

0.12

0.05

40.9

11.3

2

Associated

BC450

127.66

128.39

0.73

0.57

3.2

1.4

2.1

Associated

BC450

128.73

129.7

0.97

0.76

13.2

9.4

15.1

Associated

BC452

157.49

157.69

0.2

0.13

5.4

21.5

4.2

Associated

BC452

157.69

158.4

0.71

0.47

4.1

1.6

2.1

Associated

BC452

160.38

161

0.62

0.41

3.5

7.8

5.1

Associated

BC452

163.64

164.2

0.56

0.38

0.9

5.2

2.7

Associated

BC453

181.1

181.2

0.1

0.06

203

2.8

7.2

Associated

BC454

182.83

183.07

0.24

0.16

37.7

43.1

12.3

Associated

BC463

109.38

109.53

0.15

0.11

2

14.2

2.1

Associated

BC465

133.39

133.66

0.27

0.17

26.5

2

3

Associated

BC466A

136.22

136.54

0.32

0.24

12.4

4.4

3.1

Associated

BC468

130.32

130.61

0.29

0.22

8

4.1

2.1

Associated

BC468

164.47

164.64

0.17

0.13

1.8

16

2.9

Associated

BC469

113.38

113.81

0.43

0.27

1.3

8.3

3.1

Associated

BC469

118.43

118.95

0.52

0.32

0.6

5.8

2.6

Associated

BC469

169.64

169.92

0.28

0.18

16.6

20

6.3

Associated

BC469

170.8

171.24

0.44

0.28

37.1

6.7

8.2

Associated

BC470

189.05

189.79

0.74

0.47

17.1

3.7

6.7

Associated

BC477

210.82

211.26

0.44

0.26

0.2

8

2.8

Associated

BC481

182.2

182.6

0.4

0.21

31.4

7.9

5.9

Associated

BC481

182.6

182.9

0.3

0.16

18.6

8.4

3.4

Associated

BC481

182.9

183.15

0.25

0.13

5.3

9.5

2.1

Associated

BC481

189.23

189.93

0.7

0.37

0.8

4.2

2.2

Associated

BC481

200.8

201.06

0.26

0.14

19.8

11.6

3.6

Associated

BC481

201.23

201.45

0.22

0.12

21.7

21.5

4.7

Associated

BC482

232.73

233.08

0.35

0.15

12.8

8.8

2.9

Associated

Notes

1.   The AuEq (gold equivalent) grade is calculated using the following formula:

AuEq g per t = Au g per t + Sb% x 

Sb price per 10kg x Sb processing recovery
   Au price per g x Au processing recovery

Price assumptions are:

  • Au US$/oz = 2,500 (Au US$/gram = 80.39); and

  • Sb US$/t = 19,000 (Sb US$/10kg = 190).

Recovery assumptions are:

  • Au Recovery = 91%; and

  • Sb Recovery = 92%

The Au recovery assumption and Sb recovery assumption is based on established processing and sales in respect of Costerfield.

It is the Company’s opinion that all elements included in the metal equivalent calculation have a reasonable potential to be recovered and sold.

2.   Composites that are not interpreted to be connected to a named vein and are below 2 g/t AuEq when diluted to 1.8m are not considered significant and are not recorded here.

Drill hole collar details from modern Kendal drilling at Costerfield:

Hole ID

Northing

Easting

Elevation

Depth

Azimuth

Dip

Date Completed

AG019

6734

15206

1193

360.44

98

-41

29/01/2019

AG020

6528

15537

1195

287.68

307

-38

5/02/2019

AG023

6773

15374

959

89.66

46

5

16/09/2019

AG247W1

6454

15186

967

323.06

50

18

28/09/2025

BC001

6724

15203

1193

394.30

111

-41

8/07/2014

BC003

6873

15412

1190

160.00

98

-45

22/07/2014

BC003A

6873

15412

1190

144.40

100

-45

31/07/2014

BC004

7069

15424

1195

160.20

106

-38

11/08/2014

BC005

6988

15463

1197

90.10

103

-41

20/08/2014

BC008

6749

15635

1190

500.30

276

-38

15/12/2017

BC009

7061

15288

1192

249.90

114

-36

12/12/2017

BC010

7062

15288

1192

329.90

93

-51

3/01/2018

BC012

6770

15452

1187

251.60

285

-41

5/01/2018

BC018

6569

15261

1190

402.00

122

-61

26/02/2018

BC098

7030

15269

886

279.50

62

12

27/04/2020

BC108

7012

15354

923

229.91

46

14

3/07/2020

BC112A

6891

15357

937

170.00

93

25

29/05/2020

BC113

6890

15357

937

210.00

94

34

10/06/2020

BC114

6889

15357

938

224.80

129

36

25/06/2020

BC122

7092

15280

860

252.00

56

14

24/06/2020

BC125

6794

15380

953

60.37

65

11

8/07/2020

BC126

6794

15380

954

51.48

85

19

10/07/2020

BC128

7013

15355

925

232.30

49

34

4/08/2020

BC129

7011

15355

924

192.61

81

37

7/08/2020

BC130

7010

15354

924

215.90

109

42

13/08/2020

BC142

6751

15322

1191

208.30

121

-32

28/08/2020

BC143

6756

15322

1191

311.03

55

-31

14/09/2020

BC307

6725

15377

969

153.50

101

52

11/04/2022

BC308

6724

15377

969

150.00

78

40

16/04/2022

BC311

6879

15407

953

74.60

113

33

4/07/2022

BC312

6880

15407

953

80.90

78

16

6/07/2022

BC313

6879

15407

953

74.90

112

17

7/07/2022

BC314

6724

15377

970

150.00

69

49

18/04/2022

BC325

6725

15377

969

113.80

131

45

16/06/2022

BC326

6724

15377

969

137.30

146

35

24/06/2022

BC328

6734

15374

969

117.78

55

32

27/06/2022

BC353A

6662

15299

962

180.75

85

10

21/09/2022

BC354

6663

15299

963

202.70

58

21

18/09/2022

BC358

6659

15298

963

226.00

146

23

9/09/2022

BC359

6734

15374

969

100.10

52

30

27/09/2022

BC360

6723

15376

969

110.50

92

40

22/09/2022

BC361

6722

15375

968

73.00

119

19

24/09/2022

BC397

7012

15353

922

200.00

29

-4

29/06/2024

BC398

7012

15354

922

125.43

42

3

2/07/2024

BC404

7012

15354

923

300.07

35

10

19/07/2024

BC406

7012

15355

923

162.00

52

16

23/07/2024

BC408

7013

15353

923

216.00

40

6

16/08/2024

BC409

7012

15354

923

220.00

50

10

28/08/2024

BC414A

6759

15354

961

120.00

66

25

28/09/2024

BC415

6759

15354

961

118.45

55

15

21/09/2024

BC416

6759

15354

960

145.44

51

15

25/09/2024

BC417

6759

15353

960

194.30

43

10

16/09/2024

BC418

7013

15355

924

370.60

56

29

4/01/2025

BC419

7012

15355

925

350.30

43

21

19/01/2025

BC420

7013

15354

924

200.57

34

24

22/01/2025

BC421

7013

15353

923

390.06

24

27

1/02/2025

BC422

7013

15353

923

248.00

29

10

4/02/2025

BC423

7013

15354

924

197.20

40

26

9/02/2025

BC424

7013

15354

923

284.17

36

16

17/02/2025

BC425

7011

15355

925

162.11

67

29

12/02/2025

BC426

7013

15355

924

195.59

52

19

3/03/2025

BC427

7013

15353

924

329.10

27

20

25/02/2025

BC428

7010

15354

924

149.89

83

31

28/02/2025

BC429

7013

15353

923

250.00

23

15

7/03/2025

BC430

7012

15355

925

262.82

60

33

16/05/2025

BC431

7013

15355

924

251.43

47

26

21/05/2025

BC434

7013

15355

924

244.80

93

35

25/05/2025

BC437

6890

15358

938

147.49

86

27

7/06/2025

BC438

6889

15357

938

218.05

102

32

11/06/2025

BC439

6888

15357

939

181.20

110

37

25/06/2025

BC440

6888

15357

938

143.70

116

31

15/06/2025

BC441

6888

15356

938

194.10

132

33

19/06/2025

BC441A

6887

15356

938

149.70

130

33

21/06/2025

BC442

6888

15356

938

278.03

140

33

2/07/2025

BC443

6887

15356

938

232.92

148

31

18/08/2025

BC444

6887

15355

938

210.09

155

29

21/07/2025

BC445

7010

15354

925

221.73

100

42

1/06/2025

BC446

6891

15357

939

235.72

70

40

30/07/2025

BC447

6891

15357

939

244.74

71

34

26/07/2025

BC448

6891

15357

937

191.11

73

24

13/07/2025

BC449

6892

15356

938

229.60

32

25

14/08/2025

BC450

6890

15357

939

166.27

87

36

6/07/2025

BC451

6890

15357

938

175.65

81

30

9/07/2025

BC452

6890

15357

940

218.90

82

47

31/08/2025

BC453

6891

15357

939

222.70

58

37

3/08/2025

BC454

6891

15356

938

215.00

57

28

6/08/2025

BC455

6891

15356

937

247.00

54

20

10/08/2025

BC456

6888

15357

939

292.60

123

42

27/08/2025

BC457

6888

15356

940

280.00

139

48

23/08/2025

BC458

6887

15356

939

301.41

143

41

19/08/2025

BC459

6887

15356

939

350.23

152

37

17/10/2025

BC460

6887

15355

938

295.81

160

32

22/10/2025

BC461

6887

15356

939

233.10

139

38

5/09/2025

BC462

6888

15357

938

197.16

122

28

5/10/2025

BC463

6887

15356

937

195.87

136

25

8/10/2025

BC464

6887

15356

939

281.72

147

44

29/10/2025

BC465

6888

15356

939

277.50

130

44

2/11/2025

BC466A

6891

15357

937

250.28

59

21

20/11/2025

BC467

6891

15356

937

296.57

47

19

26/11/2025

BC468

6891

15357

938

272.08

64

30

15/11/2025

BC469

6890

15357

940

250.00

73

48

1/12/2025

BC470

6891

15357

940

256.09

62

44

6/12/2025

BC475

6887

15356

939

271.40

153

43

11/12/2025

BC476

6887

15356

939

314.47

154

39

21/12/2025

BC477

6888

15356

939

249.50

135

42

14/12/2025

BC481

6891

15357

939

277.50

55

44

2/02/2026

BC482

6892

15356

938

328.77

38

31

10/01/2026

BC483

6889

15357

940

235.00

89

50

29/12/2025

KD529

6759

15344

959

82.80

80

6

26/07/2019

KD530

6758

15344

959

81.00

103

15

28/07/2019

KD553

6765

15383

961

44.30

78

22

9/09/2019

KD556

6773

15374

958

70.00

65

-2

26/09/2019

KD557

6773

15373

958

82.00

59

12

23/09/2019

KD574

6740

15374

969

70.00

62

17

22/10/2019

KD576

6740

15374

969

90.45

40

13

23/10/2019

KD580

6795

15399

951

35.00

67

24

25/10/2019

KD588

6735

15396

970

34.90

135

11

8/11/2019

KD681

7011

15355

922

115.40

63

2

28/02/2020

KD682

7012

15355

922

127.90

54

4

3/03/2020

KD683

7012

15354

922

129.00

53

-2

10/03/2020

KD684

7012

15354

922

145.50

43

-1

30/03/2020

KD688

6824

15399

952

39.15

123

31

1/04/2020

KD696

7011

15355

923

110.10

69

16

20/04/2020

KD698

7010

15355

923

114.60

92

23

21/04/2020

KD700

7041

15339

895

150.00

48

3

18/05/2020

KD701

7009

15354

923

110.00

104

23

7/05/2020

KD702

7041

15339

895

144.00

52

9

19/05/2020

MA001

6754

15323

1191

239.53

108

-35

9/10/2020

MA002

6755

15323

1191

257.17

91

-38

3/12/2020

MA004

6753

15322

1191

256.40

118

-38

22/10/2020

MA005

6501

15531

1188

230.10

290

-41

6/11/2020

PD144

6737

15374

969

59.48

103

20

13/09/2024

PD152

6819

15413

956

12.75

110

23

17/01/2024

PD153

6819

15412

956

24.03

49

27

19/01/2024

PD220

6818

15412

956

24.40

67

28

31/05/2024

PD221A

6818

15412

957

68.23

62

38

5/06/2024

PD221AB

6818

15412

957

68.23

62

38

5/06/2024

PD222

6817

15412

956

22.83

92

46

31/05/2024

PD224

6804

15410

958

34.76

76

42

6/06/2024

PD232

6799

15410

957

20.73

164

-12

28/06/2024

PD254

6736

15374

969

90.64

51

22

2/09/2024

PD255

6736

15374

969

67.73

73

25

4/09/2024

PD256

6736

15374

969

60.00

86

22

10/09/2024

PD257

6736

15374

969

80.03

72

38

6/09/2024

TP009

6402

15270

1187

135.60

88

-45

15/02/2014

TP018

6465

15290

1188

312.60

114

-45

3/06/2014

Notes:

  1. Coordinate System: Local Costerfield Mine Grid

Appendix 2 - JORC Code, 2012 Edition – Table 1

Section 1 Sampling Techniques and Data

Criteria

JORC Code explanation

Commentary

Sampling techniques

  • Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.

  • Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.

  • Aspects of the determination of mineralisation that are Material to the Public Report.

  • In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.

Sampling of Au and Sb mineralisation is from diamond drill core (HQ2, HQ3, NQ2, BQ and LTK48) using standardised Alkane processes that have been in place for over a decade.

Due to the discrete mineralisation of the deposit, not all diamond drill core was required to be sampled. Sample intervals were determined and marked on the core by Alkane geologists using the following general rules:

  • All stibnite-bearing veins are sampled.

  • Intersections of polyphase breccias, stockwork veins, laminated quartz veins or massive quartz veins were routinely sampled.

  • A waste sample is taken either side of the mineralized vein (30–100 cm).

  • Siltstone is sampled where disseminated arsenopyrite is prevalent.

  • Fault gouge zones were sampled at the discretion of the geologist.

Diamond core sampling intervals were standardised wherever possible and ranged from 5 cm to 1 m in length. Diamond drill core samples have been cut in half using the orientation line or cut line, with a consistent side of the cut core selected for assay to ensure unbiased sampling. Whole core was sampled for LTK48 core. The methodology was validated by the Costerfield QA/QC protocols. No sampling instruments required calibration.

Drilling techniques

  • Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc.).

Diamond Drilling was undertaken using predominantly LM90 drill rigs, with NQ2 used in underground drilling and HQ2 and NQ2 on surface. HQ3 was employed where ground conditions or noise considerations required. Diamond Drilling from ore-drives and grade control drilling utilised a Kempe or Diamec rigs drilling in LTK48. A LM30 drilling BQ was used for a short period in 2020.

Core orientation was undertaken using the Axis or Reflex digital orientation kits.

Drill sample recovery

  • Method of recording and assessing core and chip sample recoveries and results assessed.

  • Measures taken to maximise sample recovery and ensure representative nature of the samples.

  • Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.

Diamond drilling was routinely checked for core loss during both drilling and sampling. Where zones of poor recovery were encountered, core loss was assigned at 0.1m intervals. Core loss blocks were added by drillers and then checked by geologists or field technicians when the core was measured, and depth marks made. If problems were encountered with recovery and core block depths, the drill shift supervisor was advised and depth marking stopped until the issue was rectified.

No relationship between grade and sample recovery has been established. Reported intervals reflect full recovery or composites with core-loss assigned a zero grade value. Mineralsiation zones with poor recovery are redrilled until a representative sample is achieved.

Logging

  • Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.

  • Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.

  • The total length and percentage of the relevant intersections logged.

All drill core was geologically logged as full core for the relevant rock quality designation, lithology, weathering, alteration, mineralsiation, structural data, and sample intervals.

Logging is qualitative in nature for the geology, and quantitative for rock quality designation.

The total length of the intersections logged is 27,688m (being 100%).

Data capture was digital into the AcQuire software using validated codes.

All drill core was photographed wet with high resolution photographs stored on the site’s server, which is routinely backed-up.

Sub-sampling techniques and sample preparation

  • If core, whether cut or sawn and whether quarter, half or all core taken.

  • If non-core, whether riffled, tube sampled, rotary split, etc., and whether sampled wet or dry.

  • For all sample types, the nature, quality and appropriateness of the sample preparation technique.

  • Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.

  • Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling.

  • Whether sample sizes are appropriate to the grain size of the material being sampled.

Diamond core sampling intervals were standardised wherever possible and ranged from 5 cm to 1 m in length. Diamond drill core samples have been pre-dominantly sampled by being cut in half using the orientation line or a cut line, with a consistent side of the cut core selected for assay to ensure unbiased sampling. Smaller diameter BQ and LTK48 core was sampled whole.

The following sample preparation activities were undertaken by Alkane staff for both diamond drill core and underground channel samples:

  • Sample information and characteristics were measured, logged, recorded in the acQuire database and assigned a unique sample ID.

  • Sample material was placed into a calico bag previously marked with the unique sample ID.

  • Calico bags were loaded into plastic bags such that the plastic bags weighed less than 10 kg.

  • An assay submission sheet was generated and placed into the plastic bag.

  • Plastic bags containing samples were sealed with a metal or plastic tie and transported to On Site in Bendigo via private courier or Alkane staff.

The following sample preparation activities were undertaken by On Site staff:

  • Samples were received and checked for labelling, missing samples, etc. against the submission sheet.

  • If the sample batch matched the submission sheet, sample metadata were entered into On Site’s LIMS. In the event that discrepancies were noted, Alkane was contacted by On Site to resolve the discrepancy prior to further work commencing. Records of all discrepancies and corrective actions taken are recorded by the Alkane database administrator.

  • A job number was assigned, and worksheets and sample bags were prepared.

  • Samples were placed in an oven and dried overnight at 106°C.

  • Samples were weighed and recorded.

  • The entire dried sample was crushed using a Rocklabs Smart BOYD Crusher RSD Combo with a jaw closed side setting of 2 mm.

  • If the dried sample weight was less than 3 kg, the entire sample was retained for pulverisation. If the dried sample weight was greater than 3 kg, the sample was spilt to 3 kg using the rotary splitter that is incorporated in the BOYD crusher.

  • Rejects from splits greater than 3 kg were retained as coarse rejects in labelled calico bags and returned to Mandalay Resources.

  • The 3 kg sample was then pulverised in an Essa LM5 Pulverising Mill to 90% passing 75 µm.

For fire assay and base metal samples:

  • The 3 kg pulverised samples were then subsampled to take a master ~200 g pulp split for assay by a manual scooping procedure across the full width and depth of the mill bowl and loaded sequentially into labelled pulp packets.

For all methods:

  • For every 21 primary samples, a sample was randomly selected by LIMS and a duplicate 200 g split for fire assay or second jar for photon assay was submitted for analysis using the same analytical procedure as the primary sample.

  • The remaining pulp was returned to its sample bag and then returned to Mandalay Resources for retention following the completion of assay.

A quarterly check-assay program is in place to monitor the representative nature of sampling and assay methodology.

Sample sizes are considered appropriate to the grain size of the material being sampled.

Quality of assay data and laboratory tests

  • The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.

  • For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.

  • Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.

The assaying protocols used at Costerfield have been developed to ensure expected levels of accuracy and precision are met for the style of mineralisation tested.

Samples were assayed for gold, antimony, arsenic, and iron using representative partial digest methodologies:

  • Gold grades were determined either by a 25g charge with lead flux fire assay and an AAS finish.

  • Antimony, iron and arsenic concentrations were determined using an aqua regia based acid digest with an AAS finish.

Assaying techniques are considered total for gold and antimony.

The quality control procedures utilised at Costerfield used CRMs prepared by commercial laboratories Geostats and OREAS.

CRMs were either prepared using Costerfield material or were otherwise matrix matched to ensure a representative nature.

At least one CRM was submitted with every batch of diamond core samples and typically at a rate of 1 standard per 25 samples. Up to six CRMs covering the expected ranges of gold and antimony mineralisation were in rotation during routine sampling.

An assay result for a CRM was considered acceptable when the returned assay fell within three standard deviations of the CRM certification grade. Outside this range, the CRM assay was considered to have failed and all significant mineralised samples within the batch were re-assayed, where significant grades were defined as mineralised samples that may have a material-impact in future resource estimates. All actions or outcomes were recorded as comments in the QA/QC register.

Alkane submitted uncrushed samples of basalt as blank material sourced from Geostats into assay sample lots, at a rate of 1 in every 30 samples, to test for contamination during sample preparation.

The failure threshold for gold is 0.10 g/t, which was chosen since it represents ten times the detection limit of 0.01 g/t for AAS. The failure threshold for antimony is 0.05%, which was chosen for being five times the detection limit of 0.01% for AAS.

Pulp duplicates were collected routinely at a rate of 1:22 by On Site and submitted with the primary sample for analysis. Precision was in line for the expected a variance in both gold and antimony.

Umpire laboratory checks to three additional commercial assay laboratories are completed each year covering all new assays generated at the property.

Verification of sampling and assaying

  • The verification of significant intersections by either independent or alternative company personnel.

  • The use of twinned holes.

  • Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.

  • Discuss any adjustment to assay data.

Sampling intervals and numbering were validated by geologists prior to cutting, with pre-numbered sampling bags systematically used by the field technicians to ensure the correct sample was submitted under each ID.

Internal validation of significant intercepts was completed by the exploration and senior geologists. Photographs, logging, sample weights and assay results were checked to ensure manual errors were eliminated.

Key intercepts at Costerfield were also validated by the Resource Geologist and Competent Person during the interpretation and modelling or the Costerfield resource estimation.

Assay and sampling data was automatically uploaded into the Acquire database system and QA/QC validated at the point of upload. Any issues were entered into a QA/QC register and resolved before data acceptance.

Alkane staff conduct periodic visits to the On Site Laboratory in Bendigo and meet regularly with the Lab managers. In early 2023 a review was conducted by a third party (RSC Consulting Pty Ltd) to ensure the practices are appropriate. Nothing of major concern was found.

Twinned holes are typically only drilled intentionally to get full recovery of an ore zone when the initial hole has core loss. There are inadvertent twinned intercepts within the database, particularly when the collar position is close to the mineralisation. Twinned intercepts provide consistent correlation of structure and mineralisation character however due to the short range grade variability common structurally controlled gold systems, may not have the same mineralisation tenor. No adjustment has been made to the assay data.

Location of data points

  • Accuracy and quality of surveys used to locate drill holes (collar and downhole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.

  • Specification of the grid system used.

  • Quality and adequacy of topographic control.

Drill hole collar locations have been determined by differential GPS or theodolite surveying methods, either by external surveyors or Alkane surveyors. A digital report is created and entered into the acQuire Database. Data entry accuracy is validated against a LiDAR topographic map and high-resolution satellite imagery. Topographic control is considered adequate.
A local mine grid system is in use at Costerfield. The MGA94 (Zone 55) coordinates can be obtained from the Costerfield Mine Grid (CMG) coordinates from the following:

MGA 'E' = (CMG 'E' x 0.945671614) - (CMG 'N' x 0.325123399) + 291068.619

MGA 'N' = (CMG 'E' x 0.325123399) + (CMG 'N' x 0.945671614) + 5905061.714

Where CMG north is +29o and +17.6 o from Magnetic North and True North respectively.

Downhole surveys were conducted using either the digital Reflex EZ-TRAC tool in both single-shot (30 m while drilling) and multi-shot mode (3 m spacing at end of hole) where required, or Axis Gyro (2024 onwards) in both over-shot and continuous modes as required.

All downhole survey data is digitally uploaded to the Reflex hub or Axis Connect respectively and automatically imported into the acQuire database.

Data spacing and distribution

  • Data spacing for reporting of Exploration Results.

  • Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.

  • Whether sample compositing has been applied.

The Kendal drilling reported in this announcement comprises infill and extension drilling at spacings that vary across the deposit as complexity dictated. In infill areas, drill spacing is approximately 40m by 40m. In extension areas, drill spacing is approximately 100m by 100m.

This approach is considered appropriate for establishing a geological and grade continuity acceptable for either an Inferred or Indicated Mineral Resource Estimation.

Where modelled veins or mineralisation zones were sub-sampled, a full-length composite of variable thickness has been reported.

Orientation of data in relation to geological structure

  • Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.

  • If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.

Drill holes at Kendal are designed to ensure an Alpha angle greater than 30°, indicating that the orientation of the drill holes (and therefore samples) are appropriate for the structure.

The drilling orientation compared to that of key mineralised structures is not considered to have introduced any sampling bias as the structures are currently interpreted.

Sample security

  • The measures taken to ensure sample security.

All drill core was delivered to the Brunswick site, which is securely gated, with video surveillance, and time stamped swipe card access.

Drill core logging and sampling was completed in this secure facility.

Sample bags containing sample material are placed in heavy duty plastic bags in which the sample submission sheet is also included. The plastic bags are sealed with a metal twisting wire or heavy-duty plastic cable ties.

The bags are taken to a storage area that is under constant surveillance.

A private courier collects samples daily and transports them directly to On Site in Bendigo, where they are accepted by laboratory personnel.

Sample pulps from On Site are returned to Alkane for storage. The pulps are stored undercover, wrapped in plastic.

Audits or reviews

  • The results of any audits or reviews of sampling techniques and data.

Internal reviews of the exploration process and procedures are completed by senior geologists.

Routine monthly lab visits and reviews are conducted by site personnel and make up part of the QA/QC protocols.

RSC Consulting Pty Ltd reviewed the sampling and QA/QC procedures and practices in early 2023. There were no major outcomes related to sampling techniques and data.


Section 2 Reporting of Exploration Results

Criteria listed in the Section 1 also apply to this section.

Criteria

JORC Code explanation

Commentary

Mineral tenement and land tenure status

  • Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.

  • The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.

Alkane manages the Costerfield Operation and holds a 100% interest in licences MIN4644, MIN5567, EL5432, EL5519, EL6842, EL6847, EL8320 and RL007485 which comprise the Property. There are no advanced projects in the immediate vicinity of the Property, and there are no other Augusta-style antimony-gold operations in production within the Costerfield district.

Drilling activities and the associated Kendal veining, this report, were located on MIN4644.

There are currently no known impediments to obtaining a licence to operate in the area. Alkane (or its predecessors) has been conducting both exploration activities and mining activities on mining lease MIN4644 since 2006.

Exploration done by other parties

  • Acknowledgment and appraisal of exploration by other parties.

The Costerfield Property has been explored using modern methods since 1966. Previous exploration by Mandalay Resources (2009–2025), prior to its merger with Alkane, represents the most significant period of exploration having discovered Cuffley, Youle and Shephard lodes in that time. No Exploration Results prior to Mandalay Resources have are reported in this release.

Geology

  • Deposit type, geological setting and style of mineralisation.

Narrow vein, antimony-gold and gold-only lodes are the targeted deposit styles at the Costerfield Property. Economic lode material consists of either a ‘typical’ gold-bearing quartz and carbonate with massive stibnite, or gold-only quartz and carbonate veining as seen in the Shepherd system. The Kendal deposit is situated in the western limb and hinge of the north-striking Costerfield Anticline, individual veins are controlled by the sub-vertical axial fabric imposed on the host siltstones during compression/folding, exploiting weakly developed cleavage and north-south shears in an approximately 50-70m wide zone. From structural observations it is currently thought that the mineralisation formed under an extensional stress regime, after the host structural framework was set up. Bedding-parallel faults with laminated quartz fill are common throughout the stratigraphic sequence and often offset individual veins westward with depth (up to 2-3m in the Kendal area), the offset being an apparent one as antimony-gold mineralisation post-dates most movement on the faults. The footwall of the Kendal system is complex, but generally lies on the No. 4 Fault which forms an anastomosing thrust ramp system with the below No. 3 Fault which breaches the Costerfield Anticline. The Kendal mineralisation progressively increases in westward dip with depth and finally becomes the Youle Lode within the No. 4 Fault.

Drill hole Information

  • A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:

    • easting and northing of the drill hole collar

    • elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar

    • dip and azimuth of the hole

    • downhole length and interception depth

    • hole length.

  • If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.

Refer to Appendix 1 for the summary of all information material to the understanding of the exploration results from the modern Kendal drilling at Costerfield.

Data aggregation methods

  • In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated.

  • Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.

  • The assumptions used for any reporting of metal equivalent values should be clearly stated.

Reported Exploration Results are intercept length weighted with no truncation of minimum and/or maximum grade applied.

Exploration Results have been reported to represent the discrete structural shear or vein as determined by the resource geologist and Competent Persons. There is no cut-off grade for the inclusion of drill intercept if it is on structure.

Aggregates are full-width of target structures/lodes and limited in true width to underground ore development widths of mining of 4.5 m and rely on structures being interpreted as parallel in orientation and representative in nature of the continuous vein.

Gold is the dominant element of value and exploration results are reported as gold equivalent (AuEq) where:



And the AuEq factor of 2.39 is calculated:

  • at a gold price of US$2,500/oz = US$80.39/gram

  • an antimony price of US$19,000/t = US$190/10kg

  • with assumed metal recoveries of 91% Au and 92% Sb.

The Au recovery assumption and Sb recovery assumption is based on established processing and sales in respect of Costerfield. All elements included in the metal equivalent calculation have an established potential to be recovered and sold.

Relationship between mineralisation widths and intercept lengths

  • These relationships are particularly important in the reporting of Exploration Results.

  • If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.

  • If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. ‘downhole length, true width not known’).

Exploration Results that have been included in this announcement have been reported as drill widths and estimated true widths. Mineralisation was modelled as sub-vertical veins that were broadly north-south in strike and consistent with historical plans and sections of the Costerfield Mine. Estimated true widths were determined from assigned dip domains for each of the modelled veins. Estimated true widths from associated mineralisation was determined using an average vein orientation of 88 degrees dip, with a dip direction of 280 degrees.

Diagrams

  • Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.

Refer to following diagrams included in the body of this announcement:

  • Figure 1 – Regional map of the Costerfield Project

  • Figure 2 – Geological cross section of the Costerfield gold-antimony vein system

  • Figure 3 – Costerfield / Kendal area plan view

  • Figure 4 – Long section of the Kendal 501 Vein

  • Figure 5 – Long section of the Kendal 520 Vein

  • Figure 8 – Cross section looking north at mine northing 7120N

  • Figure 9 – Cross section looking north at mine northing 6780N

Balanced reporting

  • Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.

For veins that are interpreted though multiple drill holes all intercepts are tabulated in Appendix 1 and illustrated in the images within the body of this announcement. Any intercepts that are not interpreted at this stage, to be part of a wider structure are tabulated in Appendix 1 if the sampled grade is above 2g/t when diluted to 1.8m.

Other substantive exploration data

  • Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.

Additional exploration data used to assist and validate interpretations at Costerfield include the use of surface geological mapping and a 2D seismic line.

Bulk density work using the immersion methodology was completed in 2021 on similar lode and waste material at the Costerfield deposit.

A regression formula is used for the BD of lode material:

Kendal:

  • If (Sb%>1) BD=((1.3951 × Sb%)+(100-(1.3951 × Sb%)))/(((1.3951 × Sb%)/4.56)+((100-(1.3951 × Sb%))/2.69) )

  • If (Sb%<1) BD= (0.05661 × Fe%) + 2.5259

Where:

  • Empirical formula of stibnite: Sb2S3.

  • Sb%: Antimony assay as a percentage by mass.

  • Molecular weight of antimony (Sb): 121.757.

  • Molecular weight of sulfur: (S): 32.066.

  • 1.3951 is a constant calculated by 339.712/243.514 where 339.712 is the molar mass of Sb2S3, and 243.514 is the molar mass of antimony contained in one mole of pure stibnite.

  • BD of pure stibnite: 4.56.

  • BD of unmineralised gangue: 2.69, representing a ratio of 1:3 siltstone to quartz.

  • Fe%: Iron assay as a percentage by mass.

The host rock BD of waste rock is 2.76 g/cm3.

There are no material occurrences of deleterious elements or contaminating substances.

Further work

  • The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling).

  • Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.

The Exploration Results reported in this document refer to areas of the Costerfield Property already in production as well as potential future production areas. Future exploration will be focused on advancing these areas through to an Indicated Resource, if drilling is successful. In addition, exploration will be conducted on the margin of currently operating areas to increase mine life where possible.

CONTACT:  NIC EARNER, MANAGING DIRECTOR & CEO, ALKANE RESOURCES LTD, TEL +61 8 9227 5677
INVESTORS & MEDIA:  NATALIE CHAPMAN, CORPORATE COMMUNICATIONS MANAGER, TEL +61 418 642 556


Images accompanying this announcement are available at

https://www.globenewswire.com/NewsRoom/AttachmentNg/fe1859e1-d5e4-4c5e-be34-91775ae5de0b

https://www.globenewswire.com/NewsRoom/AttachmentNg/bed7012e-c22b-490e-b861-333ac2c23fd3

https://www.globenewswire.com/NewsRoom/AttachmentNg/8afe8654-2c61-4fe4-9dad-213d4c6a428a

https://www.globenewswire.com/NewsRoom/AttachmentNg/fbcfab45-58bd-4719-96d7-7298ed770a75

https://www.globenewswire.com/NewsRoom/AttachmentNg/dd924b09-f601-4a6b-93b3-13c2086cd798

https://www.globenewswire.com/NewsRoom/AttachmentNg/d45c1d0e-0a1d-412d-8c57-84feff276b16

https://www.globenewswire.com/NewsRoom/AttachmentNg/278957a5-60e6-4f55-a4a8-91a489062056

https://www.globenewswire.com/NewsRoom/AttachmentNg/725cf5d1-e86b-499d-9cdc-ab303f5a21a4

https://www.globenewswire.com/NewsRoom/AttachmentNg/42f29b9e-24e8-4a5e-b7bd-976b8e7204a3

https://www.globenewswire.com/NewsRoom/AttachmentNg/a7ba9b5c-75e7-43d4-b957-d0dd3b55eb96