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Aston Bay Holdings Ltd V.BAY

Alternate Symbol(s):  ATBHF

Aston Bay Holdings Ltd. is a Canada-based mineral exploration company exploring high-grade critical and precious metal deposits. It is engaged in exploring the Storm Copper Property and Cu-Ag-Zn-Co Epworth Property in Nunavut, and the high-grade Buckingham Gold Vein in central Virginia. It is also in advanced stages of negotiation on other lands with high-grade critical metals potential in North America. The Nunavut property is located 112 km south of the community of Resolute Bay, Nunavut on western Somerset Island. The property is adjacent to tidewater on Aston Bay and comprises 12 prospecting permits and 118 contiguous mineral claims, which comprises of Storm Copper and Seal Zinc, covering an area of approximately 541,796 acres. Under Virginia property, it focuses on exploring two targets in Virginia: high-grade mesothermal gold vein mineralization along strike of the Buckingham Gold Vein and zinc-copper SEDEX-style mineralization in a newly identified base metals/polymetallic belt.


TSXV:BAY - Post by User

Post by traps7on Jan 28, 2022 3:44pm
227 Views
Post# 34372836

have Cu, especially in the feeder zone.

have Cu, especially in the feeder zone.

.......every cu,.geologist Dreams, ...of hitting a feeder zone when drilling..

..The feeder zone,..Knowen as the source,..The home run...

..Bay's Trick,  seems to have been found around the the  280m mark,..just guessing, looking at core from hole #3..Not seeing holes 1&2 so seeing hole 33 in core sample first hitting at the 185m mark which reflected the Magnetci image being highest intensity .

..just thinking,  if holes 1&2 we"er cross cutting anomaly ..then hole #3 would in-fact have been drilled into a better target after seeing Bore Hole survey"s from holes 1&2

..No sign of hole #4,..but we do see hole #5..Hole # 5 hitting at the 300 m mark same as hole #3 both showing calchopyrite..

..Hole 6,..and hole # 7 now complete both targeted the Feeder zone area looking fore size. 

..Hole # 8...Starting  .latest Tweet,.                                    .Find the Trick.....

.....Typically, SEDEXs are hosted in black shale and/or carbonate. They form from warm hypersaline fluids (~200°), that are usually oxidized (some deposits are reduced), where metals are held in chlorine complexes. The mineralization is usually layered/stratiform/stratabound. Typically only Zn+Pb mineralization, though some deposits have Cu, especially in the feeder zone. They form very big (100 mt+) deposits, but not in camps. More single large deposits spaced very far apart (20-50km) in belts. Typical setting is passive margin/failed rift/sag basin. Alteration is more subtle due to lower temperature of ore fluid - typically just carbonate.

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