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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 martindaleon Apr 13, 2023 4:02pm
102 Views
Post# 35393840

Are they still misquoting old news!

Are they still misquoting old news! Heard it all before , don’t even need to look at the post...I bet they don’t mention this part about hole 10... “
Drill Hole ST22-10 Details
 
ST22-10 targeted the margin of a large (300m x 800m), previously untested EM anomaly. The hole was drilled to a downhole depth of 382.6m and intersected both a shallow zone and deep zone of visual copper and zinc mineralization.
 
The drill hole was terminated prematurely due to a mechanical failure, with the deeper mineralized zone still open at depth.
 
The shallow mineralized zone within ST22-10 consists of 34m of weak vein style, fracture hosted and minor blebby chalcocite over a number of intervals from 17m downhole. The assays also indicate the presence of sphalerite (zinc sulfide) up to 1.05% Zn in places, and minor galena (lead sulfide).
 
The deeper zone of mineralization is over 68m thick and remains open at depth. The mineralization consists of vug, open pore space and breccia filling as well as replacement style pyrite ± chalcopyrite ± sphalerite sulfide mineralization superimposed on pre-existing hydrocarbon rich sediments. This mineralization is interpreted to be of the sediment hosted style, and distinctly different than the fault zone breccia hosted copper mineralization intersected at the 2750N and 2200N Zones at Storm.
 
Assays up to 0.44% copper (Cu) confirm the presence of chalcopyrite within the lower mineralized sequence. Zinc mineralization has also been confirmed in the lower part of the sequence with sphalerite accompanied by pyrite and calcite within bituminous vugs.”

and as usual im sure they completely forgot about the other 146? Holes... the sea of copper gravel and the 5+km of mineralization below the 7 virtually untouched plates? Nothing to see here folks... maybe they should just pack it in and go home for a few drinks... sarc... me I will wait for actual qualified people to tell me what we have here  not someone who make up facts and fake PPs and consolidations... my napkin math based on Known figures like the average grade of 2.15% in AWMs presentation and their average thickness of 24m is more than intriguing as far as I’m concerned.. listen to whoever you wish.. me I’m listening to AWMs numbers... GLTA That Deserve It... 
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