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《Geology and Prospecting》 2006-02
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MESOZOIC HYDROTHERMAL METALLOGENIC SYSTEM ANALYSIS IN THE SOUTHWEST PART OF ZHONGTIAO MOUNTAIN

XUE Ke-qin~(1,2),DENG Jun~1,SHANG Pei-lin~2,CAO Xi-lin~2(1.State Key Laboratory of Processes and Mineral Resources,China University of Geosciences,Beijing 100083;2.Geological Survey of Shanxi Province,Taiyuan 030001)  
Cu-Ni,Cu-Fe and Au deposits in the southwest part of Zhongtiao Mountain are related with Mesozoic intermediate to acidic magma activity,and belong high to low temperature hydrothermal type.Orebodies are strictly controlled by regional faulted structure,geneses of different deposits have relationship with ore source rock,such as Cu-Ni deposits hosted in metamorphic basic intrusive rock,Cu-Fe deposits in metamorphic basic volcanic rock and Au deposits in gneiss.All deposits build Mesozoic structure-magma-hydrothermal metallogenic system in the southwest part of Zhongtiao Mountain.The metallogenic system is the couple results of the same energy field,fluid field and different ore source field,and has good potential for ore prospecting.The reconnaissance of ore prospecting ought to be arranged in the area where Mesozoic middle-acid magmatic rock is distributed.
【Fund】: 国土资源大调查项目(编号:20001020150003)资助。
【CateGory Index】: P618.2
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