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大兴安岭中段二叠系地球化学特征及其成矿意义
引用本文:范书义,毛华人,张晓东,孙秀丽,李颖.大兴安岭中段二叠系地球化学特征及其成矿意义[J].地质通报,1997(1).
作者姓名:范书义  毛华人  张晓东  孙秀丽  李颖
作者单位:内蒙古地矿局115地质队
基金项目:“八五”国家科技攻关项目
摘    要:二叠纪海相火山沉积岩系是大兴安岭中段出露的主要基底地层,是铜多金属矿床的主要赋矿围岩,其中成矿元素Cu、Pb、Zn、Ag、Sn均具有较高的丰度值,是形成矿床的重要物质来源,而不同矿床类型的时、空分布与早二叠世古构造沉积环境密切相关

关 键 词:大兴安岭中段  二叠纪地层  成矿元素丰度  成矿物质来源

STRATIGRAPHIC GEOCHEMISTRY OF PERMIAN STRATA IN THE CENTRAL DA HINGGAN MOUNTAINS AND ITS METALLOGENIC SIGNIFICANCE
Fan Shuyi,Mao Huaren,Zhang Xiaodong,Sun Xiuli and Li Ying.STRATIGRAPHIC GEOCHEMISTRY OF PERMIAN STRATA IN THE CENTRAL DA HINGGAN MOUNTAINS AND ITS METALLOGENIC SIGNIFICANCE[J].Geologcal Bulletin OF China,1997(1).
Authors:Fan Shuyi  Mao Huaren  Zhang Xiaodong  Sun Xiuli and Li Ying
Abstract:The principal strata exposed in the central sector of the Da Hinggan Mountains are the Permian marine volcanic sedimentary series,which constitutes the main host rocks of copper polymetallic deposits.It has higher abundances of the ore forming elements Cu,Pb,Zn,Ag and Sn and thus is the important source of major ore forming substances.The spatial temporal distribution of different deposit types is closely related to the Early Permian tectonic sedimentary environment.
Keywords:central sector of the Da Hinggan Mountains  Permian  abundance of ore  forming elements  source of ore substances
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