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Leaching experiment research on host rocks of Qiaogashan gold deposit in Shanshan County, Xinjiang, China
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作者 ZHAI Wei, YANG Rongyong, LI Zhaolin and WU Jianjun Department of Earth Sciences, Zhougshan University, Guangzhou 510275, China State Key Laborntory of Metallogenesis, Nanjing University, Nanjing 210093, China 《Chinese Science Bulletin》 SCIE EI CAS 1999年第S2期216-218,共3页
1 Geological setting of the deposit THE Qiaogashan gold deposit is located at contact zone of middle Tianshan terrance and south Tianshanback-arc basin, and near the latter side. The orebodies are controlled by middle... 1 Geological setting of the deposit THE Qiaogashan gold deposit is located at contact zone of middle Tianshan terrance and south Tianshanback-arc basin, and near the latter side. The orebodies are controlled by middle Tianshan brittle-ductileshear zone. The main ore types are auriferous quartz veins and fractured and alterated rocks. The southpart of the deposit is hosted in striking sheared Devonian rocks, while the north part in a diorite body,which was deformed by a nape shear zone. 2 Geology and geochemistry of host rocks The host rocks of south part of the deposit are Devonian detrital stone of terrigenous origin, interlayering volcanic detrial stone of back-arc basin facies, which locally suffered intensive ductile-brittle shearing. The rock type is composed mainly of gray-green siltstone, poststone, metasiltstone, etc., and a se- 展开更多
关键词 LEACHING experiment HOST ROCKS qiaogashan gold deposit Xinjiang.
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新疆乔尕山金矿床氢、氧同位素特征及其地质意义
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作者 翟伟 李兆麟 孙晓明 《矿物岩石地球化学通报》 CAS CSCD 2001年第4期376-379,共4页
乔尕山金矿床赋存于中天山脆韧性剪切带中 ,两个主要成矿阶段成矿流体氢、氧同位素变化范围小 ,δ1 8OH2 O =5 .2 5‰~ 10 .95‰ ,δDH2 O=- 70 .9‰~ - 42 .0‰ ,成矿流体并非独立的岩浆流体与变质流体的混合。受剪切岩石组成矿物中... 乔尕山金矿床赋存于中天山脆韧性剪切带中 ,两个主要成矿阶段成矿流体氢、氧同位素变化范围小 ,δ1 8OH2 O =5 .2 5‰~ 10 .95‰ ,δDH2 O=- 70 .9‰~ - 42 .0‰ ,成矿流体并非独立的岩浆流体与变质流体的混合。受剪切岩石组成矿物中流体包裹体可能是剪切带成矿流体的主要来源之一 ,沉积岩中的同生水以及岩浆岩中的粒间溶液等者可能在剪切变质作用过程中演化为成矿流体 ,剪切作用使流体产生均一化作用形成均一的剪切带成矿流体。 展开更多
关键词 乔尕山金矿床 韧性剪切带 氢氧同位素 成矿流体
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