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一、西裘—黄砚铜矿成矿区成矿构造条件的基本特点(一) 成矿区地质概况西裘—黄砚铜矿成矿区位于临安—杭州东西构造带与绍兴—江山大断裂带的复合部位。成矿区出露地层主要有前震旦系双溪坞群(Pt_1sh)浅变质火山岩系、骆家门组(Pt_2l)滨海相碎屑岩系和震旦系下统虹赤村组(Z_1h)、志棠组(Z_1z)的浅海—滨海
First, the West Qiu - Huangyan copper ore-forming conditions of the basic characteristics of metallogenic conditions (A) the geological profile of the ore-forming area Qiu - Huangyan copper mineralization zone is located in Lin’an - Hangzhou East-West structural belt and Shaoxing - Jiangshan great fault zone composite Site. The exposed strata of the ore-forming area mainly include the former Sinian Shuangxiwu Group (Pt_1sh) super-metamorphic volcanic series, the Luojiamen Formation (Pt_2l) marine clastic series and the Sinian series Hongcicun Formation (Z_1h) and Zhitang Formation (Z_1z) shallow sea - the sea