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Tumipampa: three types of gold mineralization uncovered
Dynacor Gold Mines Inc. (dynacor) Symbol: DNG Toronto Stock Exchange (TSX)

About this update from Dynacor Group Inc
[{"type":"text","content":"\n\n\n\nDynacor Gold Mines Inc. (dynacor)\n\n\nSymbol: DNG\n\n\nToronto Stock Exchange (TSX)\n\n\nMONTREAL, July 15 /CNW Telbec/ - Dynacor Gold Mines Inc. (Dynacor\nTSX:DNG) is pleased to report the exploration results that it has obtained on\nits 100% owned Tumipampa property. In late 2007, the Company began an\n11,000 meter drilling campaign and a surface exploration programme. Initial\nresults were reported in February 2008 (see Press Release dated February 12,\n2008) and the Company now reports on all the results obtained during the first\n6 months of 2008.\n\n\nTHE TUMIPAMPA PROJECT\n\n\nThe Tumipampa project is located 500 km from the city of Lima, in the\nChapimarca district, Province of Aymaraes, Department of Apúrimac. Dynacor\nGold owns a total of 2,650 hectares which are adjacent to concessions being\nexplored by the following companies: Yamana Gold, Bear Creek and Southern\nPeru. The area is composed of quartzite (Soraya formation) and limestone\n(Ferrobamba formation) of the Cretaceous, which contain important epithermal\nAu deposits, these structures are intruded by the Apúrimac batholite, a well\nknown metallotect that is related to many porphyric Cu and Au deposits in\nPeru.\n\n\nOverall, the results obtained suggest that three different types of\nmineralization can be encountered on the Tumipampa property, namely:\n\n1. Gold bearing vein structures with variable widths ranging from 0.1 to\n 7 meters that are generally orientated along a N20degreesE/70degreesNW\n dip. The veins are mainly made-up of pyrite, chalcopyrite, hematite,\n iron oxides and grey-white quartz associated with the Soraya formation\n and the Apúrimac batholite.\n\n2. Disseminated gold mineralization associated with breccias in the\n quartzite rock.\n\n3. Gold, copper and iron mineralization associated with Skarn-type\n deposit at the interface between limestones and marbles (Ferrobamba\n formation) and the intrusive body.\n\n\nDRILLING RESULTS\n\nIn Table 1, the results for 12 drill holes are summarized including the\nveins or structures intersected.\n\n\nTABLE 1: TUMIPAMPA 2008 DIAMOND DRILLING RESULTS\n\n-------------------------------------------------------------------------\n Drill hole data\n ---------------------------------\n Drill Total Intersection\nVein hole Orienta. Inclin. length Depth (m)\n------------------------...