GEOLOGY AND GENESIS OF THE JINYING GOLD DEPOSIT IN JILIN PROVINCE
LIU Wen-xiang1, MAN Yong-lu2, WANG Xing-chang1
1. No. 602 Brigade, Jilin Bureau of Nonferrous Metallic Geology and Exploration, Baishan 134300, Jilin Province, China; 2. No. 604 Brigade, Jilin Bureau of Nonferrous Metallic Geology and Exploration, Huadian 132400, Jilin Province, China
Abstract：The Jinying gold deposit in Baishan City, Jilin Province is tectonically located in the northeastern margin of Liaodong anteclise, Sino-Korean metaplatform. It occurs in the silicified tectonic breccia belt between the Neoproterozoic Diaoyutai quartzose sandstone and the Paleoproterozoic Zhenzhumen silicated dolomitic marble. The orebodies are jointly controlled by the regional fault F102 and local fault F100. The special forming environment and physical-chemical conditions make its unique assemblage of minerals and texture of ores. This deposit belongs to a new type recently found in China, the Mesozoic orogenic type.
刘文香, 满永路, 王兴昌. 吉林省白山市金英金矿床地质特征及成因探讨[J]. 地质与资源, 2009, 18(4): 279-283.
LIU Wen-xiang, MAN Yong-lu, WANG Xing-chang. GEOLOGY AND GENESIS OF THE JINYING GOLD DEPOSIT IN JILIN PROVINCE. GEOLOGY AND RESOURCES, 2009, 18(4): 279-283.
2009, Vol. 18 
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