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锡铁山铅锌矿床成矿构造背景
引用本文:吴冠斌,孙华山,冯志兴,樊俊昌,陆建培,王玉奇.锡铁山铅锌矿床成矿构造背景[J].地球化学,2010,39(3):229-239.
作者姓名:吴冠斌  孙华山  冯志兴  樊俊昌  陆建培  王玉奇
作者单位:1. 中国地质大学资源学院,湖北,武汉,430074
2. 西部矿业股份有限公司,青海,西宁,810001
基金项目:中央高校基本科研业务费特色团队项目 
摘    要:以锡铁山地区滩间山群火山-沉积岩为研究对象,利用岩石学和地球化学方法,探讨了滩间山群火山-沉积岩的成岩构造背景,旨在制约锡铁山铅锌矿床的成矿构造背景。结果表明,滩间山群火山-沉积岩的成岩构造背景为弧后盆地,且在地球化学方面,表现出从弧后盆地拉张初期至成熟期的连续演化特征。而锡铁山铅锌矿床则于弧后盆地拉张初期形成。

关 键 词:弧后盆地  成矿构造背景  滩间山群  锡铁山

The paleotectonic setting of Xitieshan lead-zinc deposit
WU Guan-bin,SUN Hua-shan,FENG Zhi-xing,FAN Jun-chang,LU Jian-pei,WANG Yu-qi.The paleotectonic setting of Xitieshan lead-zinc deposit[J].Geochimica,2010,39(3):229-239.
Authors:WU Guan-bin  SUN Hua-shan  FENG Zhi-xing  FAN Jun-chang  LU Jian-pei  WANG Yu-qi
Institution:WU Guan-bin1,SUN Hua-shan1*,FENG Zhi-xing2,FAN Jun-chang2,LU Jian-pei1 and WANG Yu-qi1 1. Faculty of Resources,China University of Geosciences,Wuhan 430074,China,2. Western Mining Co. Ltd,Xining 810001
Abstract:The tectonic setting of volcanic and sedimentary rocks of the Tanjianshan Group in the Xitieshan region was studied using geologic and geochemical methods, aiming at better constraints on the tectonic setting of the Xitieshan lead-zinc deposit. The results show that the Tanjianshan Group formed in a back-arc basin environment. Moreover, geochemical results show continuous characteristics, from juvenile back-arc basin to mature. However, the Xitieshan lead-zinc deposit was formed at the early stage of the ba...
Keywords:back-arc basin  tectonic setting of mineralization  Tanjianshan Group  Xitieshan  
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