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Decade Resources Ltd V.DEC

Alternate Symbol(s):  DECXF

Decade Resources Ltd. is a Canadian based mineral exploration company seeking opportunities in the resource sector. The Company holds numerous properties at various stages of development and exploration from basic grass roots to advanced ones. Its properties and projects are all located in the Golden Triangle area of northern British Columbia. Its projects include Grassy, Premier East, Red Cliff, Lord Nelson, Del Norte and Terrace. The Terrace project includes Terrace Gold, Kleanza, Dardanelle, Treasure Mountain and Nobody Knows. The Company owns 100% of Goat property. The Copper River Valley properties are comprised of three main claim blocks; Terrace Gold-Darranelle-Treasure Mountain group of claims located in northern British Columbia. The property consists of 52 contiguous mineral claims. The Grassy property contains approximately 830.20 hectares in two separate claims which are owned 100% by the Company. The Red Cliff project consists of approximately eight mineral claims.


TSXV:DEC - Post by User

Bullboard Posts
Post by stockgod3on Jan 18, 2016 2:15pm
113 Views
Post# 24469466

Bids are Building For Some Reason? Whats Cooking?

Bids are Building For Some Reason? Whats Cooking?NEWS RELEASE---SULPHURETS REGION IN BC’S GOLDEN TRIANGLE GAINS PROMINENCE January 18, 2016, Vancouver, BC: Teuton Resources Corp. (“Teuton”) (“TUO”-TSX-V) ("TFE"- Frankfurt) (“TEUTF”—OTCBB) reports that the Sulphurets region, centered on Seabridge Gold’s KSM property and Pretium Resources’ Brucejack property (with northern and southern extensions covered by many Teuton properties), is becoming recognized as one of the great mineral provinces of the world. A recent Northern Miner article entitled “Pretium explores porphyry potential at Brucejack” compares the region to Grasberg, Indonesia: Warwick Board, chief geologist at Pretium Resources (TSX: PVG; NYSE: PVG), says excitement is building for exploration at the company’s Brucejack project in northwestern B.C., as his team zeroes in on discoveries within a district that compares in metal content to Grasberg, the world’s largest gold mine in Indonesia. “One of the things I always thought about before I moved to Canada is just how spectacular the rest of the Cordillera is from Chile, Peru and to Arizona,” Board tells The Northern Miner during a phone interview. “At the time it didn’t make sense why we’re not finding the same mineral wealth here in Canada, but now I think, ‘Wow, we’re on the edge of finding another massive mineral province with big potential.’” [https://www.northernminer.com/news/pretium-explores-deep-porphyry-potential-atbrucejack/1003744653/]. The sentiment is also echoed by Jeff Kyba, Northwest Regional Geologist for the British Columbia government: “Over the past five years, the northwest Stikine has built its momentum towards becoming the world’s next big mineral province,” he says. “People are recognizing that these deposits have high-grade roots and big extensions they never thought were there.” [BC Survey's 'red line' a game changer for explorers. Northern Miner, May 6, 2015. https://www.northernminer.com/news/bcgs-presents-a-big-gamechanger-for-explorers-in-nw-stikine/1003601910/?&er=NA#sthash.8QptB20p.dpuf] Warwick Board has theorized that the gold-rich structures currently being developed for production at Pretium’s VOK gold deposit may be related to a porphyry system at depth: Based on indications from drill core and surface data, Board reckons that Brucejack — and the other gold-rich veins exuding out to surface — may be the golden branches of a much larger porphyry deposit hidden beneath. “There’s something driving Brucejack, these systems don’t exist in isolation, and there’s certainly a lot of rusted rock out there,” he says. The article goes on to say: “In recent years, Pretium has come to understand the role of Devonian-aged structures in directing porphyry and epithermal deposits into the crust, and the trail of breadcrumbs it has left for B.C. explorers to follow. Unfortunately, most of these structures today are hidden from view, Board explains, largely overprinted by later deformation events during the Cretaceous, when the margin of western North America collided with the outboard terranes. “During island arc development there were earthquakes going on, and that created the structural plumbing needed to promote emplacement of metal-rich magmas,” he says. “What we see in the camp is a distinct north–south trend in mineralization, and that highlights where
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