In summary, the Project hosts a numbers of narrow massive sulphide lenses along a folded horizon. The "A", "C", "E" and "O" zones host historic mineral resources; whereas the "B" and "D" zones have no mineral resources. The two other lenses, the "F" and "V" appear independent from the others but possibly along the same trend.
Fancamp's exploration efforts were focused on increasing the size of the mineralized system and the Company succeeded in extending the mineralization southwards albeit along narrower intervals than was intersected in the historical Namex drilling. The northern extent appears truncated by a fault. At this time, Fancamp does not plan any further field work but will commence a more in-depth compilation-synthesis-analysis of the Clinton-Namex data package and to determine if the Project may hold a 5 to 25 million tonnes base and precious metal mineral resources.
The technical information in this news release was compiled, reviewed and approved by Jean Bernard, P. Geo., the Company's Senior Geologist, and Jean Lafleur, P. Geo., President and CEO and a Director of the Company. Both individuals are Qualified Persons under NI 43-101 Rules.
Diamond Drill Hole Statistics from the 2010-2012 Exploration Work by Fancamp Exploration Ltd., on the Clinton Copper-Zinc Project------------------------------------------------------------------ Diamond Drill UTM Azimuth/ Hole Coordinates Dip LengthYear Zone # NAD 83, Zone 19 (degrees) (m) ---------------------- Easting Northing------------------------------------------------------------------2010 South CL-2010-01 344932 5022836 110/-50 237 ------------------------------------------------------- CL-2010-02 344932 5022836 110/-68 168 ------------------------------------------------------- CL-2010-03 344152 5023594 110/-50 108 ------------------------------------------------------- CL-2010-04 344114 5023467 110/-50 141 ------------------------------------------------------------- Total 654 m------------------------------------------------------------------2011 "D" CL-2011-01 349929 5033238 102/-45 209 ------------------------------------------------------- CL-2011-02 349928 5033238 102/-61 222 ------------------------------------------------------- CL-2011-03 349908 5033149 102/-45 213 ------------------------------------------------------- CL-2011-04 349908 5033149 102/-61 252 ------------------------------------------------------- CL-2011-05 349898 5033067 102/-50 198 ------------------------------------------------------- CL-2011-06 349898 5033067 102/-65 225 ------------------------------------------------------------- "V" CL-2011-07 350739 5032816 110/-45 228 ------------------------------------------------------- CL-2011-08 350769 5033021 110/-45 189 ------------------------------------------------------- CL-2011-09 350290 5033017 110/-45 240 ------------------------------------------------------- CL-2011-10 349247 5031735 115/-45 69 ------------------------------------------------------- CL-2011-11 349340 5031911 115/-45 66 ------------------------------------------------------- CL-2011-12 349549 5032097 115/-45 150 ------------------------------------------------------------- Total 2,255 m------------------------------------------------------------------2012 South CL-2012-01 346436 5026254 110/-50 123 ------------------------------------------------------------- "F" CL-2012-09 348928 5030218 106/-45 228 ------------------------------------------------------- CL-2012-10 348928 5030221 106/-65 207 ------------------------------------------------------- CL-2012-11 348476 5030381 110/-45 126 ------------------------------------------------------- CL-2012-12 348502 5031303 110/-45 144 ------------------------------------------------------- CL-2012-18 348411 5031342 110/-45 261 ------------------------------------------------------------- "D" CL-2012-02 349975 5033036 95/-45 126 ------------------------------------------------------- CL-2012-03 349879 5032968 98/-50 204 ------------------------------------------------------- CL-2012-04 349879 5032968 98/-65 274 ------------------------------------------------------- CL-2012-05 349844 5033187 102/-55 321 ------------------------------------------------------- CL-2012-06 349990 5033133 102/-55 123 ------------------------------------------------------- CL-2012-07 349929 5033238 95/-61 261 ------------------------------------------------------- CL-2012-08 350009 5033221 93/-45 132 ------------------------------------------------------------- "V" CL-2012-13 350727 5033161 107/-70 300 ------------------------------------------------------- CL-2012-14 350673 5033023 107/-68 324 ------------------------------------------------------- CL-2012-15 350778 5033144 112/-68 249 ------------------------------------------------------- CL-2012-16 350813 5033134 110/-68 132 ------------------------------------------------------- CL-2012-17 350679 5032986 102/-68 305 ------------------------------------------------------- CL-2012-19 350668 5032959 110/-68 342 ------------------------------------------------------- CL-2012-20 350606 5033016 110/-65 387 ------------------------------------------------------- CL-2012-21 350568 5032961 110/-65 432 ------------------------------------------------------- CL-2012-22 350273 5033032 110/-65 264 ------------------------------------------------------- CL-2012-23 350717 5033090 85/-55 246 ------------------------------------------------------- CL-2012-24 350451 5033272 110/-60 231 ------------------------------------------------------------- Total 5,742 m------------------------------------------------------------------
Quality Assurance / Quality Control Protocols
Drill core boxes from the 2010, 2011 and 2012 diamond drilling campaigns arrived at the Fancamp core logging facility located in Thetford Mines (Quebec). Boxes are opened and depth tags are verified for errors. Each box is labeled with embossed aluminum tape stapled to box end. Numbers indicated hole and box numbers as well as "from" and "to" footages. Sampling is continuous through mineralized intervals and intermittent in other lithologies or lithological contacts. Within mineralized intervals, samples taken are between 0.5 to 1.0 meters in length of half-sawed core, or up to lithological or structural boundaries.
According the nature of the mineralization, whether Gold, Copper and/or Zinc, one to three standards per hole are included within the sampling of mineralized zones (ME-7, CDN-ME-14, P4A). One blank sample is inserted at every 17 to 19 samples. The blank sample used is a pure quartzite from Lac Daveault (Quebec).
Other parameters described in the drill logs included structure, alteration and mineralization. Mineralization is described as a visual percentage of sulphides. Sample bags are wrapped with scotch tape. Samples are placed in large rice bags for shipping, all secured with a cable tie. Samples are transported from the core shack to the Thetford Mines bus station. They are shipped by commercial transport to the ALS Laboratory Group facilities in Val-d'Or (Quebec) (the "ALS Laboratory"). Shipping waybills and sample submittal form are scanned and sent to the lab by internet. They are also kept for tracking shipments as required.
Samples arriving at the ALS Laboratory are individually weighed, dried at high temperature, crushed 70% to less than 2 millimeters, riffle split and pulverized 85% to less than 75 micrometre. Samples were analyzed by the Au-ICP 21 and ME-MS41 methods. If values returned greater than 100 g/t Silver, 10,000 ppm Copper and 10,000ppm Zinc for the ME-MS41 assay method, then a second assay is done using the either Ag-OG46, Cu-OG46 and/or Zn-OG46 method.
S.E.C. Exemption: 12(g)3-2(b)
Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this news release.
Contacts:
Fancamp Exploration Ltd.
Jean Lafleur, M. Sc., P. Geo.
President and CEO
(514) 975-3633
pjlexpl@videotron.ca
www.fancampexplorationltd.ca
Bay Street Connect
Michael D'Amico
Investor Relations
(647) 500-6023
michael@baystreetconnect.com
