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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 copper and gold deposits in Virginia, United States, and Nunavut, Canada. The Company is exploring the high-grade Buckingham Gold Vein in central Virginia and is in advanced stages of negotiations on other lands with high-grade copper potential in the area. The Company is focused on its Blue Ridge Project in Virginia. The Nunavut Property is 100% owned by the Company and located 112 kilometers (km) south of the community of Resolute Bay, Nunavut on western Somerset Island. The Storm Copper Project is located on Somerset Island, Nunavut, approximately 20 km from tidewater at the Company. Its Seal Zinc deposit is located at the base of a small peninsula approximately 350 meters from tidewater at its on Somerset Island, Nunavut. Its Mountain Base Metals Project is located on 2,072 acres of private land with direct access to both highway and rail transportation.


TSXV:BAY - Post by User

Post by martindaleon Apr 13, 2023 4:02pm
83 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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