Is ZEN a Unique, One of a Kind Flake Deposit?...I believe it is, after all it's "
completely different to common flake graphite", and "the rarest form of graphite known to man”.
Yes, the Albany seems to be the rarest form of Flake deposit on Earth and known to man.
It contains coarse to fine FLAKE graphite in its core, and although the_Chief would like everyone to believe that lump has flake graphite in it, it just isn't that simple.
You see, all graphite when milled shows its flake structure, but that's after milling. Please don't take my word for it, read it for yourself:
https://asbury.com/technical-presentations-papers/materials-in-depth/vein-graphite/
As with all graphite materials the micro-morphology of vein graphite converges to flake structure as the particle size is decreased. This convergence is illustrated by the accompanying series of scanning electron micrographs of Asbury grade 98DC milled vein graphite:
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So after studying the core back in Feb. 2012, Prof. Dr. Andrew Conly of Lakehead University, confirmed the core contained coarse, medium and fine FLAKE GRAPHITE.
But the_Chief says Lump has Flake Graphite. Really? I thought Lump when milled and broken down to smaller sizes, only then does it show its FLAKE structure.
So how did Prof. Dr. Andrew Conly confirm the presence of FLAKE GRAPHITE in the Albany core back in Feb. 2012?
Is it maybe because Albany is a very unique, very rare, one of a kind, FLAKE DEPOSIT?
No fargen way says the_Chief, lol. I say it is. JMO but you be the judge:
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Eveleigh and his team sent off samples to the local university and within a few weeks, they received results that forced them to rethink their entire company strategy. Theprofessor told them they had found “the rarest form of graphite known to man”. It was a “volcanic setting; vein or hydrothermal style” kind of graphite found in meteorites and the earth’s mantle – completely different to common flake graphite
Now here is the news stating the University findings that proclaims Albany to be hydrothermal, and yet has
Course Size FLAKE from the drill core.
So, don't laugh because the professor from his findings and metalurgical testing found that the core was from a hydrothermal source, and yet FLAKE was used to describe the graphite.
Here's the link:
https://bolsa.diariodeleon.es/noticias-actualidad/marketwire/en-Zenyatta-Ventures-University-Study-Shows-Positive-Results-from-Graphite-Deposit-Confirms-Presence--769331001.html
Zenyatta Ventures; University Study Shows Positive Results from Graphite Deposit; Confirms Presence of Coarse Flake Graphite
Marketwire
lunes, 27 febrero 2012
THUNDER BAY, ONTARIO -- (Marketwire) -- 02/27/12 -- Zenyatta Ventures Ltd. ("Zenyatta" or "Company") (TSX VENTURE:ZEN) is pleased to provide results from an independent mineralogical study of drill core samples from the newly discovered Albany Graphite Deposit located near Hearst in north-eastern Ontario. The following significant observations were made:
-- Flake sizes of coarse, medium and fine ranging from 50 to greater than
300 microns (-270 to +40 mesh size)
-- Characterized as a magmatic hydrothermal style of graphite
mineralization (similar to the high value Sri Lankan type deposits)
-- Graphite represents essentially all of the total reported Carbon assay
values (i.e. Carbon related to carbonate is less than 1%)
Aubrey Eveleigh, President and CEO stated "Zenyatta management considers these latest results to be very important, especially the range in flake size, which includes the high value coarse flake. Coarse flake graphite is greater than 175 microns (or +80 mesh) in size. Flake size and purity are key parameters in establishing the potential value and marketability of any graphite product derived from the Albany Graphite Deposit. The Company is planning to conduct metallurgical testing of the graphite zones and carry out a more aggressive drilling campaign to determine the full extent of the deposit".
The mineralogical report was prepared by Dr. Andrew Conly, Ph.D. of Lakehead University Mineralogy and Experimental Laboratory ("LUMINX") in Thunder Bay, Ontario. The petrographic observations were from four samples of the graphite-rich breccia in zone #2 of drill hole Z11-4F1.
As previously announced in the Company's news release dated 19 January 2012, a recent drill hole on the Albany project testing a large airborne EM conductor measuring 1400 metres by 800 metres, intersected eight (8) separate and extensive graphite-rich breccia zones. The geophysical anomaly was explained by the conductive graphite matrix which is highly unusual in character and size. Core photos, section and maps can be seen on the website at www.zenyatta.ca and will also be available for viewing in the Core Shack at the PDAC on Sunday and Monday. The following lists the results for total carbon ("C") from each of the zones, which are believed to represent true width (in metres):
Zone 1 - 79.8 - 89.7 yielded 4.6% C over 9.9m;
Zone 2 - 112.5 - 180.0 yielded 4.2% C over 67.5m;
Zone 3 - 183.1 - 191.0 yielded 3.3% C over 7.9m;
Zone 4 - 329.5 - 377.7 yielded 2.5% C over 48.2m;
Zone 5 - 411.0 - 437.4 yielded 3.0% C over 26.4m;
Zone 6 - 467.3 - 472.8 yielded 4.2% C over 5.5m;
Zone 7 - 481.0 - 488.5 yielded 2.1% C over 7.5m;
Zone 8 - 506.0 - 522.0 yielded 3.0% C over 16.0m
The graphite discovery is located 30km north of the Trans Canada Highway and a gas pipeline. A rail line is located 70km away and an all-weather road approximately 4-5km from the graphite deposit. The deposit is near surface, underneath glacial till overburden.
A similar deposit may be the vein graphite deposits of Sri Lanka. Vein graphite has been interpreted as being derived by hydrothermal fluids, as in the Albany Graphite Deposit. The origin of the graphite is proposed to be derived from a CO2 rich fluid, likely related to the emplacement of a carbonatite. This CO2 rich fluid could promote hydraulic fracturing (brecciation) and precipitation of vein graphite. Graphite veins and breccias are quite rare, and very few are described in the geologic literature.
The Bogala Mine, a Sri Lankan graphite deposit, has been in production since 1847. It is a high grade, narrow vein (20cm), underground mine. Sri Lankan graphite still enjoys great demand due to its unusually high purity and unique physical properties.
The outlook for the global graphite market is very promising with demand growing rapidly from new applications in clean technology including fuel cells, solar panels and rechargeable batteries. China produces over 70% of global supply and, like other commodities, now has less available for export as domestic demand grows. As global demand outstrips supply, graphite prices have increased substantially, more than doubling over the past three years.
Graphite is a natural form of carbon with the chemical formula C, which it shares with diamond and coal. It is now considered one of the more strategic elements by many leading industrial nations, particularly for its growing importance in high technology manufacturing and in the emerging "green" industries, such as hybrid vehicle components. The application for graphitic material is constantly evolving due to its unique chemical, electrical and thermal properties. It maintains its stability and strength under temperatures in excess of 3,500 degrees C and is very resistant to chemical corrosion. It is also one of the lightest of all reinforcing elements and has high natural lubricating abilities. Some of these key physical and chemical properties make it critical to modern industry.
Mr. Aubrey Eveleigh, P.Geo., President and CEO, is the "Qualified Person" under NI 43-101 and has reviewed the technical information contained in this news release. Analyses was carried out by ALS Chemex Labs using a total carbon (LECO) method code of C-IR07 and a multi element package ICP-MS with code ME-MS81.
This News Release includes certain "forward-looking statements". These statements are based on information currently available to the Company and the Company provides no assurance that actual results will meet management's expectations. Forward-looking statements include estimates and statements that describe the Company's future plans, objectives or goals, including words to the effect that the Company or management expects a stated condition or result to occur. Forward-looking statements may be identified by such terms as "believes", "anticipates", "expects", "estimates", "may", "could", "would", "will", or "plan". Since forward-looking statements are based on assumptions and address future events and conditions, by their very nature they involve inherent risks and uncertainties. Actual results relating to, among other things, results of exploration, project development, reclamation and capital costs of the Company's mineral properties, and the Company's financial condition and prospects, could differ materially from those currently anticipated in such statements for many reasons such as: changes in general economic conditions and conditions in the financial markets; changes in demand and prices for minerals; litigation, legislative, environmental and other judicial, regulatory, political and competitive developments; technological and operational difficulties encountered in connection with the activities of the Company; and other matters discussed in this news release. This list is not exhaustive of the factors that may affect any of the Company's forward-looking statements. These and other factors should be considered carefully and readers should not place undue reliance on the Company's forward-looking statements. The Company does not undertake to update any forward-looking statement that may be made from time to time by the Company or on its behalf, except in accordance with applicable securities laws.
Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Contacts:
Zenyatta Ventures Ltd.
807-346-1660
info@zenyatta.ca
www.zenyatta.ca
Read more at
https://www.stockhouse.com/companies/bullboard/v.zen/zenyatta-ventures-inc?postid=21746335#1Y6ctAluKQyPJAZt.99