Kenorland Minerals Ltd. · TSXV:KLD
Kenorland Minerals — Technical Presentation (January 2021)
15 slides from Kenorland Minerals's technical presentation, January 2021
Slide 1: Hunter Project – January 2021
Hunter Project – January 2021
Slide 2: Disclaimer and Qualified Person
Disclaimer and Qualified Person The information contained herein, while obtained from sources which we believe are reliable, is not guaranteed as to its accuracy or completeness. References are made herein to historical information containing geologic and technical information. By its nature, this i
Slide 3: Abitibi Greenstone Belt Geology
Abitibi Greenstone Belt Geology • Abitibi Greenstone Belt (AGB) is the ONTARIO QUEBEC 2nd largest Au-endowed district in the world (~280 Moz endowment) • AGB also one of the largest VMS districts in the world (>750 Mt endowment) • Two distinct styles of Au mineralization: orogenic Au & intrusion-rel
Slide 4: Magnetics
Abitibi Greenstone Belt Magnetics • Curvilinear E-W trending ONTARIO QUEBEC deformation zones expressed as major lineaments in magnetic data control much of the orogenic gold endowment • Early syn-volcanic aged Au deposits also found proximal to major E-W deformation zones • The Hunter Project is si
Slide 5: Gravity
Abitibi Greenstone Belt Gravity • Gravity – Bouger anomaly map with ONTARIO QUEBEC high-pass filter applied to enhance upper-crustal contrasts • Steep gravity gradients are located along the length of major E-W trending deformation zones representing steep, deep-penetrating structures prospective fo
Slide 6: Volcanic Assemblages
Abitibi Greenstone Belt Volcanic Assemblages • Most of the VMS camps in the ONTARIO QUEBEC northern Abitibi are located on the Deloro – Stoughton-Roquemaure stratigraphic contact • Deloro to Stoughton-Roquemaure transition is a rifted arc setting • Rifted arcs have been found to have more precious m
Slide 7: Syn-volcanic plutons with VMS/porphyry systems
Abitibi Greenstone Belt Syn-volcanic plutons with VMS/porphyry systems • Hunter Exploration Target: syn- ONTARIO volcanic intrusion-related Au and Au- QUEBEC rich VMS • All syn-volcanic intrusions associated with Au-VMS, porphyry-Au, and base metal VMS have a mafic component (i.e. diorite or gabbro)
Slide 8: Calderas
Abitibi Greenstone Belt Calderas • Five recognized calderas in the ONTARIO QUEBEC Abitibi (Selbaie, Gemini, Normetal, Hunter, and Noranda) Selbaie caldera – 2728 Ma • All of the recognized caldera systems host significant mineral deposits Gemini caldera – 2735 Ma • Calderas form in calc-alkaline set
Slide 9: Geology
Hunter Geology • The underlying geology of the Hunter property is dominantly felsic volcanics and volcaniclastics of the Deloro volcanic assemblage ONTARIO QUEBEC – Flanked by the syn-volcanic Poularies pluton (diorite- granite-tonalite-trondhjemite) to the east and surrounded by Stoughton-Roquemaur
Slide 10: Drilling
Hunter Drilling • 169 DDH holes on property (26,519m) – 48 DDH holes part of Colonisation program (3,763m) – 30 DDH holes directly on strike ONTARIO of Hunter Mine (8,179m) QUEBEC – Only 31 DDH holes testing the remainder of the felsic volcanics package (6,400m) • The Hunter Project remains largely
Slide 11: Mineral Occurrences & Au in tills (HMC)
Hunter Mineral Occurrences & Au in tills (HMC) Mineralized/Altered zone Ice direction • Mineral occurrences have been • Up to 40m wide carb-sil-ser-chl alteration zones found within the Hunter project area • 1 – 10m zones up to 30% py +/- cpy-sph-mt in stringers and disseminated by previous explorer
Slide 12: HMC Drill-for-Till compilation
Hunter HMC Drill-for-Till compilation Au – HMC Assay Cu – HMC Assay • Au is highly anomalous in all sample media Ice direction from historic drill-for-till sampling completed in the 1980’s • HMC Assays – 4000 ppb Au is the 98th percentile for till samples in the Abitibi (from Kenorland’s database of
Slide 13: Comparisons Au in HMC till samples
Hunter Comparisons Au in HMC till samples Ice direction • Au in HMC assays at Hunter are comparable to other major gold Ice direction deposits in the Superior province • The Casa Berardi and Rainy River gold deposits were identified using drill-for-till methodology Rainy River Duparquet ~5 Moz Au @
Slide 14: Comparisons Au in fine-fraction (-63um) till samples
Hunter Comparisons Au in fine-fraction (-63um) till samples • Au in fine fraction geochemistry is comparable to major deposits such Ice direction Ice direction as Troilus, Eleonore, and Kenorland’s Regnault prospect • All of these deposits/prospects have clusters of >50 ppb Au in -63um fine Troilus
Slide 15: Surficial Geology
Hunter Surficial Geology • Majority of the property is covered in glaciolacustrine clay that inhibits all surface geochemical exploration for gold ONTARIO QUEBEC • Average overburden thickness – 18m • This is an advantage – if there was an outcropping major deposit in the area it would have been fou
Kenorland Minerals — Technical Presentation (January 2021) on 6ix