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《Geological Review》 1985-04
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METALLOGENIC CONDITIONS OF THE ZHILINGTOU GOLD—SIL VER DEPOSIT IN ZHEJIANG PROVINCE

Liang Zihao;Zhu Qingtao;Han Menghe;Xia Anning;Wang Yanbin;Yu Wenjuan;Zhang Yinzhen Zhejiang Institute of Geological Sciences Laboratory of Zhejiang Bureau of Geology and Mineral Resources  
The Zhilingtou gold-silver deposit is located in the southwestern segment ofthe Chencai-Suichang uplift zone between the Yuyao-Lishui and Shaoxing-Jiang-shan deep fractures. There are two structural layers in the ore district. The basement is representedby metamorphic rocks of the pre-Ordovician Chencai Group, consisting mainly ofbiotite-plagioclase gneiss with garnet-biotite-plagioclase gneiss. The cover is repre-sented by volcanic rocks of the Upper Jurassic Mushishui Formation,including tuff,rhyolite and subvolcanic rocks, which overlies the basement unconformably. The orebodies occur as veins and are strictly controlled by the NE-trendingtenso-shear basement fracture. The principal ore minerals include electrum, kustelite,argentite, hessite, pyrite, galena, sphalerite, pyrrhotite and chalcopyrite. The gangueminerals comprise quartz, chlorite, rhodonite, calcite, rhodochrosite and garnet. Thewell-rock alteration include silicification, sericitization, pyritization and chloritiza-tion. The formation of the deposit may be divided into two metallogenic epochs.The early mineralization occurred in the Caledonian cycle and is associated withthe Caledonian regional metamorohism. This is the most important metallogenicepoch of gold and silver mineralizations. The late mineralization occurred in theYanshian cycle, mainly manifested by overprinting of Ag, Pb and Zn mineraliza-tions, which are related to volcanic activity. The mineralizations of the two metallo-genic epochs show obvious differences in mineralogy, fluid inclusions and stableisotopic composition. The deposit was formed by overprinting of metamoiphichydrothermal fluids and volcanic hydrothermal fluids.
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Chinese Journal Full-text Database 10 Hits
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