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《JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY》 1995-01
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A NEW FINDING IN GEOLOGY THROUGH GEOELECTRIC SECTION OF YONGCHANG-DUQING MOUNTAIN IN GANSU

Shi Yingjun; Zhang Chaowen; Cun Shucang  
MT section of Yongchang-Duqing Mountain in Gansu can be divided into four lithologicelectrical layers and two groups of the structure-electrical layers. The latter is located in the top and inner of the base of Pre-Changcheng system, respectively. It develops shrike faults but no deep fractures. It is formed by two groups of nappe-slip structure, one is shallower, another is deeper. The ore-bearing ultrabasic body of sulphide copper-nickel ore deposits in Jinchang is pulled from south to north and from deep to shallow by the nappe-slip structure. It has no root and no connection with the deep thoroushfare.
【CateGory Index】: P631.322
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【Citations】
Chinese Journal Full-text Database 1 Hits
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【Co-citations】
Chinese Journal Full-text Database 10 Hits
1 WU YUN-FEI TAN QI-JIA (Northwest Plateau Institute of Biology, Academia Sinica, Qinghai, Xining);CHARACTERISTICS OF THE FISH-FAUNA OF THE CHARACTERISTICS OF QINGHAI-XlZANG PLATEAU AND ITS GEOLOGICAL DISTRIBUTION AND FORMATION[J];Acta Zoologica Sinica;1991-02
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【Secondary Citations】
Chinese Journal Full-text Database 6 Hits
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