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《Geotectonica Et Metallogenia》 2008-03
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METALLOGENIC POTENTIALITY OF GUAISHISHAN CU-NI MINERALIZED BASIC-ULTRABASIC ROCKS IN BEISHAN AREA,GANSU PROVINCE

WANG Lishe1,2,YANG Jianguo2,XIE Chunlin2,WANG Yuxi2,LEI Yongxiao2,CAO Hongxia1,YANG Pengfei2 and QI Yalin3(1.MOE Key Laboratory of Continental Dynamics,Northwest University,Xi'an 710069,Shaanxi,China;2.Xi'an Geological Survey Center,Xi'an 710054,Shaanxi,China;3.Research Institute of Changqing Oil Field,Xi'an 710021,Shaanxi,China)  
In order to research the metallogenic potentiality of Cu-Ni sulfide for the Guaishishan basic-ultrabasic rocks in Beishan area,Gansu,field investigation and indoor research has been carried out and the conclusions could be summarized as follows:1)The Guaishishan rock body is a complex which is composed of olivine websterites,olivine orthopyroxenites,pyroxenites and gabbros.The olivine websterites are mineralized with Cu(0.1%-0.24%)and Ni(0.12%-0.47%).2)The major and trace elements of the rocks have the characteristics of island arc ultrabasic rocks,such as low Nb,Ta,Ti,Hf,Y,P but higher Ba,Rb,Th,U,K,La contents.3)The anomaly extensions for electromagnetism fits mineralized rocks on the surface and show that there are more mineralized bodies in the depth(the maximum intensity of magnetic filed is up to 1210.96nT;the highest electric polarization is up to 9.55%,anomaly area is 500m×200m).4)Rock geochemical characteristics of the Guaishishan body are similar to those of the Jinchuan,Halatongke,Hongqiling deposits,and especially identical to those of Heishan deposits.Thus,mineral reserves of the Guaishishan Cu-Ni sulfide deposit may be more than that in the Heishan(Gansu).Besides,some clues for Cu-Ni sulfide deposit prospecting in the Beishan area has been put forward.
【Fund】: 中国地质地调查局战略性矿产远景调查项目(K47E015001 K47E016001);; 中央地质勘查基金2007年度地质矿产勘查项目(2007651139).
【CateGory Index】: P612
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