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论断陷槽中的铜镍硫化物矿床
引用本文:郝梓国,王希斌,鲍佩声,毛景文,乔德武.论断陷槽中的铜镍硫化物矿床[J].地质找矿论丛,1992,7(1):52-62.
作者姓名:郝梓国  王希斌  鲍佩声  毛景文  乔德武
作者单位:中国地质科学院,中国地质科学院,中国地质科学院,中国地质科学院,中国非金属矿工业公司 北京,北京,北京,北京
摘    要:

关 键 词:断陷槽  铜矿  镍矿  硫化物  矿床

ON DISCUSSION OF THE COPPER-NICKEL SULPHIDE DEPOSITS IN THE DEEP-FAULTING GEOSYNCLINE
Hao Ziguo,Wang Xibin,Bao Peisheng,Mao Jingwen and Qiao Dewu.ON DISCUSSION OF THE COPPER-NICKEL SULPHIDE DEPOSITS IN THE DEEP-FAULTING GEOSYNCLINE[J].Contributions to Geology and Mineral Resources Research,1992,7(1):52-62.
Authors:Hao Ziguo  Wang Xibin  Bao Peisheng  Mao Jingwen and Qiao Dewu
Institution:Institute of Geology, Chinese Academy of Geological Science, Beijing, 100037;Institute of Geology, Chinese Academy of Geological Science, Beijing, 100037;Institute of Geology, Chinese Academy of Geological Science, Beijing, 100037;Institute of Geology, Chinese Academy of Geological Science, Beijing, 100037;China National Non-metallic Minerals Industry Corporation
Abstract:Copper-nickel sulphide deposits in the deep-faulting geosyncline locating along passive continental margin are peculiar nickel deposit type in China. Now, 4 deep-faulting geosyncline and their metallogenic belts have been divided in the orogenic zone of China. On the basis of types of ore-bearing rock bodies, 4 ore deposit types are differentiated in the metallogenic belts. There are unique rock associations, rock chemistries, rock-forming minerals and component in different kind of nickel deposit. According to their characteristics genetic mechanism and minerogenetic pattern are put forward with relevant geological signs of minerogenetie prediction.
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