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《Geology and Exploration》 2010-05
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Geological Features and Geodynamic Background of the Molybdenum Polymetallic Deposits in Central-Western Inner Mongolia

HOU Wan-rong1,2,NIE Feng-jun1,XU Bin2,3,LI Wei4,FAN Yong-wei5,ZHAO Chun-rong2(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;2.The First Gold General Party of CAPF,Harbin 150086;3.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083;4.Xinda Gold Mining Limited Company of China National Gold Group Corporationy,Baotao 014060;5.No.2 Gold Geological Party of CAPF,Huhhot 010010)  
A series of molybdenum or molybdenum polymetallic deposits have been discovered in central and western Inner Mongolia recent years,such as the Bainaimiao Cu(Mo,Au) deposit in Siziwangqi county,Dasuji Mo deposit in Zhuozi county,Xishadegai Mo deposit in Wulateqianqi county,Liubagou and Hadamengou Au(Mo) deposit in Baotou city,Chaganhua Mo(W) deposit in Wulatehouqi county,Liushashan Mo(Au) deposit in Ejinaqi county.These findings provide broad prospects for prospecting molybdenum or molybdenum polymetallic ore deposits in these areas.They have also broaden exploration visions and added new research contents for geological scholars.In this paper we make a preliminary summary of the geological background,geological features,genetic types,spatial-temporal distribution characteristics and evolution of mineralization of these deposits for the first time,and briefly discussed the relationship between molybdenum,copper-molybdenum-gold,molybdenum-bismuth-tungsten,molybdenum-gold mineralization and tectonic-magmatic activity.The Liubagou and Hadamengou gold-molybdenum deposits,and Bainaimiao copper-molybdenum-gold deposits occurred in the Archean,Proterozoic metamorphic rock formation,whereas the Xishadegai molybdenum deposit,Dasuji molybdenum deposit,Chaganhua molybdenum-tungsten deposit,and Liushashan molybdenum-gold deposit respectively appeared in the Hercynian-Indonisian granite.Although,geological settings and geographical locations of these deposits have some differences,they are closely related to granitoid intrusions (dyke) in space,belong to molybdenum or molybdenum polymetallic deposits related to the intermediate-acidic hypabyssal intrusive rocks (porphyry) or plutonic intrusive rocks.In addition,according to the spatial distribution features,these deposits (occurrences) can be divided into five molybdenum or molybdenum polymetallic mineralized concentration areas in the study region:They are the Dasuji-Mingxinggou molybdenum concentration area,Bainaimiao-Gunawusu Copper-molybdenum-gold mineralized concentration area,Hadamengou-Sadegai gold-molybdenum mineralized concentration area,Manitu-Chaganhua molybdenum-bismuth-tungsten mineralized concentration area and Liushashan-Heiyingshan molybdenum-gold mineralized concentration area.The formation of these molybdenum polymetallic deposits is closely related to tectonic-magmatic events induced by the plate subduction,collision and suturing,and the deposits are the products of crustal tectonic-magmatic activities at specific evolutionary stages.
【Fund】: 危机矿山接替资源找矿项目(编号:20089948)资助
【CateGory Index】: P618.65
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