Abstract：Located in the convergence zone of India plate, Tarim-Sino-Korean paleoplate and Siberia ancient plate, Xinjiang has complicated geological structure. With an analysis of the characteristics of large deformation as a starting point, this paper comprehensively summed up such characteristics of the large-scale deformation structure as its type, size, pattern, material composition, structural order and deformation stage, discussed the control role of the large-scale deformation structure over stratigraphic framework, magmatic activities, metamorphism and deformation, regional tectonic evolution and metallogenesis, and divided the tectonics into 34 large deformation structures. The relationship between the evolution of large-scale deformation structure and the mineralization was tentatively investigated.
董连慧 王克卓 朱志新 赵同阳 郑加行 徐仕琪. 新疆大型变形构造特征与成矿关系研究[J]. 中国地质, 2013, 40(5): 1552-1568.
DONG Lian-hui, WANG Ke-zhuo, ZHU Zhi-xin, ZHAO Tong-yang, XU Shi-qi, ZHENG Jia-xing. The relationship between the characteristics of the large-scale deformation structure and the metallogenic processes in Xinjiang[J]. Geology in China, 2013, 40(5): 1552-1568(in Chinese with English abstract).