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《Mineral Deposits》 2008-06
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Skarnization of Qianhe structural alteration type gold deposit in Henan Province and its ore-prospecting significance

WANG ZaiCong1,2,LI ShengRong3 and SHEN JunFeng3 (1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2 Graduate School of Chinese Academy of Sciences,Beijing 100049,China; 3 State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China)  
The Qianhe gold deposit in the Xiong'ershan area of Henan Province was previously regarded as a hydrothermal alteration-type gold deposit. Gold mineralization is strictly controlled by fractures and hosted in meta-andesitic rocks of the Middle-Proterozoic Xiong'er Group which has undergone low-greenschist facies regional metamorphism. It is notable that some skarn minerals such as garnet,diopside,epidote,chlorite and actionlite were locally discovered in the Shijialing segment of the Qianhe gold deposit in recent years,suggesting typical skarn-forming processes of prograde,retrograde and sulfide stages with relative reduction characteristics. In addition,the wall rocks of Qianhe skarn are meta-andesitic rocks rather than carbonates. The Qianhe skarn mine-rals might result from the interaction of hydrothermal fluids derived from the near-by Heyu granite plutonism with meta-andesites of the Xiong'er Group,and their development is valuable to the understanding of Qianhe gold mineralizeation as well as to the follow-up exploration in this area.
【Fund】: 河南省嵩县前河金矿成矿规律研究与深部预测项目的资助
【CateGory Index】: P618.51
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