蒙古中部巴彦洪古尔蛇绿岩带乌兰布拉格新块状硫化物矿床
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引用本文:D. DORJNAMJAA,Ts. AMARSAIKHAN,B. ENKHBAATAR,G. ALTANSHAGAI.2012.蒙古中部巴彦洪古尔蛇绿岩带乌兰布拉格新块状硫化物矿床[J].地球学报,33(s1):9-11.
DOI:10.3975/cagsb.2012.s1.06
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作者单位E-mail
D. DORJNAMJAA Paleontological Center, Mongolian Academy of Sciences ddorj2001@yahoo.com 
Ts. AMARSAIKHAN Paleontological Center, Mongolian Academy of Sciences  
B. ENKHBAATAR Paleontological Center, Mongolian Academy of Sciences  
G. ALTANSHAGAI Paleontological Center, Mongolian Academy of Sciences  
中文摘要:The Bayankhongor ophiolite zone, a NW-SE strik-ing linear structure 400 km long and up to 25 km wide, is the largest ophiolite association in Central Mongolia and possibly in all of Central Asia. The Bayankhongor cop-per mineralization was investigated by us in connection with detailed research of the ophiolite complexes in 1997-2011. With regard to their origin the ore formations belong to genetic type of gold-bearing massive sulphide deposit with magmatic seat of the island arc.
中文关键词:massive sulphide deposit  Bayankhongor ophiolite zone  central Mongolia
 
New Ulanbulag Massive Sulphide Deposit in the Bayankhongor Ophiolite Zone, Central Mongolia
Abstract:The Bayankhongor ophiolite zone, a NW-SE strik-ing linear structure 400 km long and up to 25 km wide, is the largest ophiolite association in Central Mongolia and possibly in all of Central Asia. The Bayankhongor cop-per mineralization was investigated by us in connection with detailed research of the ophiolite complexes in 1997-2011. With regard to their origin the ore formations belong to genetic type of gold-bearing massive sulphide deposit with magmatic seat of the island arc.
keywords:massive sulphide deposit  Bayankhongor ophiolite zone  central Mongolia
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