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青海夺确壳金矿地质特征
引用本文:徐新文,史生清.青海夺确壳金矿地质特征[J].青海大学学报,2009,27(2).
作者姓名:徐新文  史生清
作者单位:徐新文,XU Xin-wen(青海省核工业地质局,青海,西宁,810008);史生清,SHI Sheng-qing(青海省有色地勘局八队,青海,西宁,810000)  
摘    要:阐述了青海省泽库县夺确壳金矿床地质特征。矿区共发现独立矿床(点)6个,构造破碎蚀变带9条,圈定大小金矿体(脉)50多条。成矿期为印支期。矿床成因类型为中低温热液型,工业类型属构造蚀变岩型矿床。主要找矿方向为夺确壳4Au2异常区和外围8Au3异常区及深部。

关 键 词:夺确壳金矿  地质特征  地球化学特征  找矿标志  找矿方向

Geological characteristics of Duoqueke gold deposit in Qinghai province
XU Xin-wen,SHI Sheng-qing.Geological characteristics of Duoqueke gold deposit in Qinghai province[J].Journal of Qinghai University(Natural Science),2009,27(2).
Authors:XU Xin-wen  SHI Sheng-qing
Institution:1.Qinghai Provincial Bureau of Nuclear Geology;Xining 810008;China;2.Qinghai Provincial Bureau of Nonferfros Metal and Geological Mineral Exploration;Eighth Party;Xining 810000;China
Abstract:Duogueke gold deposit is located in the Zeke county of Qinghai province and where,6 pieces independence deposits(spots),9 structure fracture alteration belts and more than 50 strips of gold reefs has been discovered.The ore-forming period is in the Indosinian stage,genesis classification is medium-low temperature hydrothermal type and industry classification belongs to the structure alteration rock type.The main prospectiong divection is in the Duoqueke 4Au2 and 8Au3 geochemical anomaly area and depths.
Keywords:Duoqueke  gold deposit  geological characteristic  geochemical characteristic  prospecting sigh  prospecting direction  
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