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内蒙古乌拉特后旗查干德尔斯钼矿床地质特征及Re-Os测年
引用本文:蔡明海,彭振安,屈文俊,贺钟银,冯罡,张诗启,徐明,陈艳.内蒙古乌拉特后旗查干德尔斯钼矿床地质特征及Re-Os测年[J].矿床地质,2011,30(3):377-384.
作者姓名:蔡明海  彭振安  屈文俊  贺钟银  冯罡  张诗启  徐明  陈艳
作者单位:1. 广西大学资源与冶金学院,广西南宁,530004
2. 国家地质实验测试中心,北京,100037
3. 内蒙古自治区第八地质矿产勘查开发院,内蒙古乌海,016000
基金项目:本文得到内蒙古自治区地质矿产勘查开发局“内蒙古自治区内生金属成矿规律及靶区筛选(ND2007004)”项目的资助
摘    要:查干德尔斯钼矿床是近年来在内蒙古西部中蒙边境地区新发现的一个具大型规模的隐伏矿床,辉钼矿化呈浸染状、团块状、细脉状分布在中细粒二长花岗岩中,具斑岩型矿床的特点.笔者在矿区成矿岩体、矿化和蚀变特征等初步研究的基础上,进行了辉钼矿Re-Os测年,获得模式年龄为(240.3±3.9)~(244.2±3.5)Ma,等时线年龄为...

关 键 词:地质学  矿床特征  Re-Os测年  查干德尔斯钼矿  内蒙古西部地区

Geological characteristics and Re-Os dating of molybdenites in Chagandeersi molybdenum deposit, western Inner Mongolia
CAI MingHai,PENG ZhenAn,QU WenJun,HE ZhongYin,FENG Gang,ZHANG ShiQi,XU Ming,CHEN Yan.Geological characteristics and Re-Os dating of molybdenites in Chagandeersi molybdenum deposit, western Inner Mongolia[J].Mineral Deposits,2011,30(3):377-384.
Authors:CAI MingHai  PENG ZhenAn  QU WenJun  HE ZhongYin  FENG Gang  ZHANG ShiQi  XU Ming  CHEN Yan
Institution:CAI MingHai1,PENG ZhenAn1,QU WenJun2,HE ZhongYin3,FENG Gang3,ZHANG ShiQi1,XU Ming1 and CHEN Yan1(1 College of Resource and Metallurgy,Guangxi University,Nanning 530004,Guangxi,China,2 National Research Center for Geoanalysis,Beijing 100037,3 No.8 Geological Party of Inner Mongolia Bureau of Geology and Mineral Resources Exploration and Development,Wuhai 016000,Inner Mongolia,China)
Abstract:The Changandeersi molybdenum deposit is a concealed large-size molybdenum deposit newly discovered in western Inner Mongolia. It is a porphyry molybdenum deposit characterized by disseminated, spot and veinlet mineralizations hosted in medium-fine grained monzonitic granite. Re-Os isotopic dating of seven samples from various ore bodies of the ore deposit yields model ages between (240.3±3.9) Ma and (244.2±3.5) Ma, and isochron age of (243.0±2.2) Ma, with initial 187Os being (-0.3±2.4) and MSWD being 0.78, indicating that molybdenum mineralization took place in Triassic and had a association with tectonomagmatic orogenic process in Indosinian period. The Ejin Banner-Urad Rear Banner-Sonid Left Banner belt in western Inner Mongolia near the Sino-Mongolian boundary is considered to be a molybdenum-polymetallic ore belt. The characteristics of granites related to mineralization and molybdenum deposits in this ore belt and the prospecting criteria are summed up in this paper.
Keywords:geology  characteristics of ore deposit  Re-Os isotopic age  Chagandeersi molybdenum deposit  western Inner Mongolia
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