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《Geology in China》 2013-05
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The crystal forms and thermoelectricity of pyrite from the Shuangwang gold deposit, Shaanxi Province and their applications to metallogenic prognosis

ZHANG Fang-fang;WANG Jian-ping;LIU Chong-hao;CAO Rui-rong;CHENG Jian-jun;YANG Yong-rong;QI Feng;WANG Luo;State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences;Shaanxi Taibai Gold Mining Co., Ltd.;  
Pyrite is one of the most important gold-bearing minerals, and its crystal forms and thermoelectricity have important implications to the prospecting and evaluation of gold deposits. Based on systematic sampling from drill holes ZK18, ZK30 and ZK40 in the Shuangwang breccias-type gold deposit, the authors mainly studied the crystal forms and thermoelectricity of pyrite, and have reached the following conclusions. The crystal forms of pyrite are fairly simple, comprising cube, octahedron, pentagonal dodecahedron and their composite combination, with the main crystal habit being {hk0}. Overall, the number of crystal forms is in decreasing order of {hk0}, {100}, {111}. The thermoelectric conductive type of pyrite is mainly N-P type, with the thermoelectric coefficients of Ntype pyrite ranging from-322.0 to-1.7μV·℃-1and those of P-type pyrite ranging from 1.7 to 346.7μV·℃-1; the thermoelectric parameters of pyrite vary greatly; the degree of denudation varies from 53.67% to 60.12%. All of the above data indicate a better exploration prospect at the depth of drill holes ZK18, ZK30 and ZK40 in No. 9 and No. 8 ore bodies.
【Fund】: 国家自然科学基金项目(41030423、41272106);; 中国黄金集团公司科技项目“陕西省太白县双王金矿床地质特征、成矿规律及找矿靶区再研究”共同资助
【CateGory Index】: P618.31
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