| OH-K | Potassium Feldspar | PEGMATITE | WYOMING |
Geology:
Plutonic environment of monzonite suites.
Deposit may indeed be pegmatitic though the OH-K deposit lacks the quartz cap and zonation typical of the region and pegmatitic deposit structure. Host rock is in the monzonite clan, that here is k-spar rich, also called granophyre. Estimated to be 1 to 2 sq. mile surface exposure. Host granophyre is a dense pink color due to the large amount of spar present and is in the Grade 2 category for feldspar/syenite. Host granite at 75% k-spar by volume and covers an area of up to several sq. miles.
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Mineralization:
Includes PURE K-SPAR CORE (200' x 35' x 25' OUTCROP) with few quartz clots. The quartz clots have no great vertical extent and may be the roots of the cap if one did exist; largest clot sise was as 2x2x1 feet, a dozen or less are seen of these inclusions in the core.
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Work:
New discovery; only hand-work such as trenching, mapping and sampling
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Results:
Pure core with outcrop of 75,000t and up to >10 Mmt of ore occurring as the host granophyre. No by-products apparent.
USGS conducted ORE-GRADE ASSAY
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Property Details & Access:
100 acres
Access to 1/4 mile of the core is from 1k of dirt
road from pavement; 4x4 able to reach core terrain.
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Detail Location:
N Rocky Mtn. region, nearist town Buffalo
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Other Comments:
New Discovery!! Very high-grade k-spar deposit of world-class potential.
Being recent and unworked discovery this large deposit is very rich in k-spar.
Feldspar demand rising.
PRICE $500,000 CASH & PART TRADE
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Vendor / Contact:
Email: srites@sprintpcs.com
Phone: 541-337-2212
nwyom01Submitted 08/09
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