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Fancamp Exploration Ltd V.FNC

Alternate Symbol(s):  FNCJF

Fancamp Exploration Ltd. is a Canadian mineral exploration company. The Company is focused on strategic interests in its high potential mineral projects, royalty portfolio and mineral properties. The Company is focused on an advanced asset play with a portfolio of mineral claims across Ontario and Quebec, Canada, including copper, gold, zinc, titanium, chromium, strategic rare-earth metals, and others. It has investments in an existing iron ore operation in the Quebec-Labrador Trough, a rare earth elements company, NeoTerrex Minerals Inc., in addition to an investment in a zinc mine in Nova Scotia. It is developing an energy reduction and titanium waste recycling technology with its advanced titanium extraction strategy. Its properties include Clinton Property, Stoke Property, DiLeo Property, Grasset Property, Riley Brook property, Gaspe Bay Group Property (including Boisbuisson and St. Marguerite), and other properties. The Clinton Property is located in the Appalachian region.


TSXV:FNC - Post by User

Bullboard Posts
Comment by Sunnybrook25on Dec 26, 2014 12:35pm
398 Views
Post# 23265696

RE:RE:400 ton bulk sample

RE:RE:400 ton bulk sampleA drilling program was also recently completed on the Robidoux property. A total of 795 metres of NQ drilling in nine drill holes was completed on Dec. 10, 2014. The program tested the A zone vein to vertical depths of 35 to 155 metres and a splay fault hosting a feeder vein to the A zone to vertical depths of 30 to 70 metres. Analytical results are expected in January, 2015. The A zone vein was intersected in all five holes drilled on the vein, with true widths estimated to vary from 10 centimetres to 0.8 metre. The four holes drilled on the splay fault feeder zone showed a complex relationship of folded and faulted veins, vein fragments, and stockworks and breccias within graphitic to silicified siltstones to mudstones locally showing cataclasite textures. Visible gold was observed in these four holes, particularly in samples showing crack and seal textures. Drilling on this structural corridor was over a strike distance of 80 metres and across widths in the order of five to 10 metres. Core recovery was poor in some intervals, particularly closer to surface. The high-grade quartz boulders reported in the news release of Oct. 22 appear to have originated from this splay fault feeder zone.
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