Business
CADILLAC MINING CORP. ANNOUNCES RESULTS FROM BREAK PROJECT DRILLING
CADILLAC MINING CORP. ANNOUNCES RESULTS FROM BREAK PROJECT DRILLING
About this update from Copper Quest Exploration Inc.
[{"type":"text","content":"\n\n\n\n Sep. 13, 2010 (Canada NewsWire Group) -- \n\nTR.cnwUnderlinedCell TD {\n BORDER-BOTTOM: #000000 1px solid\n}\nTR.cnwDoubleUnderlinedCell TD {\n BORDER-BOTTOM: #000000 3px double\n}\nTR.cnwBoldUnderlinedCell TD {\n BORDER-BOTTOM: #000000 3px solid\n}\nTD.cnwUnderlinedCell {\n BORDER-BOTTOM: #000000 1px solid\n}\nTD.cnwDoubleUnderlinedCell {\n BORDER-BOTTOM: #000000 3px double\n}\nTD.cnwBoldUnderlinedCell {\n BORDER-BOTTOM: #000000 3px solid\n}\n\n\n VANCOUVER, Sept. 13 /CNW/ - Cadillac Mining Corporation (TSXV:CQX)\n announces that all assay results have now been received for the\n 830-meter drill program recently completed on its Cadillac Break\n properties located near Rouyn-Noranda, Quebec.  Three diamond drill\n holes were completed on two separate target areas.\n \n\n Wasa Project\n \n\n DDH CM06-12, cored to 383 meters in August of 2006 in unexplored ground\n covered by glacial drift, identified weak but significant copper and\n zinc mineralization in the bottom 83 meters of the hole.  Cadillac\n re-entered this hole and extended it to a final depth of 596 meters,\n where uniform low-grade base metal values persist to EOH.  Coring from\n 300 meters to the bottom of the hole intersected variably textured\n chloritic alteration, possibly of basaltic origin, that carries strongly\n anomalous copper and zinc values over the entire interval.   Analytical\n results from 330.5m to 593.4m (262.9 meters) average 267ppm and 279ppm,\n copper and zinc respectively.  This includes sections from 351.2 to\n 362.0 (10.8 meters) carrying 1250ppm (0.125%) and from 372.1 to 377.3\n (5.2 meters) of 2050ppm (0.205%) copper.  Zinc values range between 200\n and 500ppm.\n \n\n This approximately 300-meter thick altered zone is comprised of mafic\n flows, with tuffaceous sections, and minor felsic to mafic intrusions. \n All display strong chloritic alteration with broad zones of banded black\n chlorite, and no detectable destructive foliation.  Pyrite content is\n generally low, ranging from trace to 5%.  While none of the intercepts\n are of economic tenor, this zone is interpreted as a feeder system\n typical of those seen under volcanogenic massive sulphide (VMS) systems\n in the Noranda Camp.\n \n\n The Wasa property lies at the intersection of the Horne Creek and\n Beauchastel faults, whi...