Lying in the north margin of Talimu plate, the East Tianshan Mountain has very complicated tectonic background. As there exist remarkable differences in tectonic evolution, magmatic activity, geochemical environment, strata and structural distribution in different parts of the area, geochemical division of the area into subareas should be performed. Four geochemical subareas were distinguished in the study area, i.e., Dananhu islend arc, Xiaorequanzi interarc basin, Kangguer ductile shear deformation belt, and Yamansu back-arc basin. Distribution of Cu, Au high values shows that their ore-forming processes and enrichment are rather complex. The study of these problems has laid a solid foundation for the determination of geochemical backgrounds and thresholds as well as the integrated ore prognosis.
崔彬, 和志军, 赵磊, 董连慧, 刘拓, 屈君. 东天山中段地球化学分区及其特征[J]. 物探与化探, 2008, 32(5): 488-491,513.
CUI Bin, HE Zhi-jun, ZHAO Lei, DONG Lian-hui, LIU Tuo, QU Jun . GEOCHEMICAL SUBAREAS OF THE MIDDLE PART OF EAST TIANSHAN MOUNTAIN AND THEIR CHARACTERISTICS. Geophysical and Geochemical Exploration, 2008, 32(5): 488-491,513.
[1] 白云来.新疆东部梧桐窝子群的大地构造背景及其地球化学论证[J].新疆地质,1994,12(2):106.
[2] 崔彬,李忠.物质场—能量场—空间场综合成矿预测[J].现代地质,1998(4):46.
[3] 花林宝,阳翔,钟华.新疆东天山沙泉子地区地球化学特征及找矿预测[J].矿产与地质,2002,16(92):291.
[4] 姜立丰,姬厚贵,郑勇.新疆东天山区域构造演化与矿产资源潜力分析//东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议.2001.
[5] Zhai Y S,Deng J.An outline of mineral resources of China and their tectonic setting[J].Austrian Journal of Earth Sciencs,1996,43:673.