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Shot Rock Phase I Drilling to Resume Post Pause
Shot Rock Phase I Drilling to Resume Post Pause Canada NewsWire OTTAWA, March 23...
About this update from Northern Shield Resources Inc.
[{"type":"text","content":"\n\n\n\nShot Rock Phase I Drilling to Resume Post Pause\n\n/* Style Definitions */\nspan.prnews_span\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\na.prnews_a\n{\ncolor:blue;\n}\nli.prnews_li\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\np.prnews_p\n{\nfont-size:0.62em;\nfont-family:\"Arial\";\ncolor:black;\nmargin:0in;\n}\n.prntar{\nTEXT-ALIGN: RIGHT\n}\n\n\n\n\n\n\n\nCanada NewsWire\nOTTAWA, March 23, 2020\n\n\n\nGeophysics Points Toward System Continuing to Depth\n OTTAWA, March 23, 2020 /CNW/ - Northern Shield Resources Inc. (\"Northern Shield\" or the \"Company\") (TSXV: NRN) is pleased to provide an update on the inaugural drilling program at the Shot Rock Property (\"Shot Rock\") in Nova Scotia, Canada. Shot Rock is being explored for low sulphidation epithermal (LSE) type gold.\n\n \n \n \n \n \n \n\n \nTo date, eight drill-holes totalling approximately 2,189 metres of the planned 2,000 to 2,500 metre diamond drilling program have been completed at the Highway Zone. Drilling has focussed on areas of near surface alteration and veining. In light of the global COVID-19 pandemic, management felt that it was prudent to allow contractors to return home to be with their families during the COVID-19 pandemic, while travel conditions still allowed. Further drilling is planned subsequent to the receipt of assays.\n\"While we are encouraged by the early visual observations of our Phase I drill program at Shot Rock, management is focused on the safety and security of its personnel during this unusual period. This pause will also allow our team to incorporate future assays in our attempt to vector into a potential discovery. Drilling will resume when it has been deemed safe to do so.\"\n-       Ian Bliss, President & CEO\nMuch of the alteration and veining intersected in the first phase of drilling is hosted in a series of gabbro dykes. The epithermal fluids appear to be exploiting the same structural weaknesses as the dykes which are easily fractured and infiltrated by the fluids due to their brittle nature. During the alteration process, magnetite is converted to hematite and other non-magnetic minerals causing the altered dykes to have a markedly lower magnetic signature than their unaltered counterparts. Such magnetite destruction processes are commonly seen in ...