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J4 ›› 2006, Vol. 14 ›› Issue (6): 24-28.
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ZHANG Huaquan,ZHU Hongling
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Abstract:
The Xilaokou gold deposit is located in the east to Guocheng fault.The deposit occurs in the intersection between the Linlong monzonite granite bodies of new Proterozoic Sinian period and the Jinshan stratum of ancient Proterozoic.The ore bodies are controled by NE and nearly EW trend faults.They formed with lens shape and with pyritization,silication and carbonation alternation.Because of the difference of ore-controlling structure and their wall rocks characteristic,the deposit bed types are divided into pyrite sericite-quartz type and multi-metal sulfide type.Its prospecting direction is pointed out.
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ZHANG Hua-Quan, SHU Hong-Ling. Geological features and its prospecting direction of Xilaokou gold deposit in Yushan city,Shngdong province[J].J4, 2006, 14(6): 24-28.
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http://www.goldsci.ac.cn/EN/Y2006/V14/I6/24
[1]沈远超,刘铁兵,刘厚民,等.山东海阳郭城金矿床地球化学特征及成因[J],地质与勘探,2001,37(1):39-42. [2]刘玉强,刘殿浩,于志臣,等.胶莱盆地东北缘金矿床主要类型与成矿远景评价[J],山东地质,2000,16(1):29-37. [3]罗忠明.山东牟平辽上金矿床地质特征[J],2000,16(3):22-25.
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