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SKRR Exploration Drill Program Intersects Significant Quartz Veining at the Irving-Leland Gold Property

Vancouver, British Columbia--(Newsfile Corp. - February 10, 2021) - SKRR Exploration Inc. ( TS...

articleSkrr Exploration, Inc.February 10, 20215/company/skrr-exploration-inc/news/skrr-exploration-drill-program-intersects-significant-quartz-veining-at-the-irving-leland-gold-property
SKRR Exploration Drill Program Intersects Significant Quartz Veining at the Irving-Leland Gold Property

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[{"type":"text","content":"SKRR Exploration Drill Program Intersects Significant Quartz Veining at the Irving-Leland Gold PropertyVancouver, British Columbia--(Newsfile Corp. - February 10, 2021) - SKRR Exploration Inc. (TSXV: SKRR) (OTC Pink: SKKRF) (FSE: B04Q) (\"SKRR\" or the \"Company\") is pleased to announce that it has intersected quartz veining at shallow depth in the first 3 holes completed during the current winter drill program at the Irving-Leland property (the \"Irving-Leland Property\"), in the Trans Hudson Corridor, Saskatchewan.Sherman Dahl, chief executive officer of SKRR, comments, \"The drill program at the Irving-Leland property is advancing well and we are encouraged by the visual mineralization and the indication of quartz veining. Assays are pending. We look forward to building off this success in the remaining 6 holes of this winter program.\"Highlights:Hole LE21001 - The hole targeted mineralization at depth beneath the surface Michelle showing. The hole collared in metagabbro which continued to 36.1m and transitioned to a diorite down to 131.5m, again grading to a metagabbro until the end of the hole. 1 m wide interval of milky white to blue quartz vein was intersected from 12.24m to 13.24m. The quartz vein had up to 2% sulphide mineralization consisting of semi-massive pyrite and pyrrhotite with trace chalcopyrite.Hole LE21002 - The hole was stepped back on section from LE21001 and targeted beneath the NW Irving and Michelle trenches. The hole intersected fine grained mafic meta volcanics to 41.1m grading to fine grained amphibolite from 41.1m to 112.5m and into a Diorite from 112.5m to end of hole. Two mineralized quartz veins were associated with the amphibolite - diorite contact, notably; 104.54m a 25cm semi-translucent to milky white quartz vein with 0.5% pyrite and trace pyrrhotite and 112.29m a 21cm semi-translucent to milky white quartz vein with 0.5% combined pyrrhotite and chalcopyrite blebs.Hole LE21003 - The hole was collared tot the east of LE210002 and drilled to the west beneath the Irving showing. The hole encountered mafic metavolcanics from 8.1m to 25.4m grading to a medium grained amphibolite from 25.4m to 73.9m then alternating sequences of Diorite to mafic metavolcanics from 73.9m to end of hole. From 46.25m to 47.6m the interval contained up to 1-2% discontinuous mineralized quartz veins of 1-2cm scale with ...

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