• 责任者：Zheng Jianjing （Institute of Geology and Geophysics ; Chinese Academy of Sciences ; Lanzhou 730000 ; China） ; Su Long
• 刊名：Geotectonica et Metallogenia
• 出版年：2009
• 卷期：33(1)
• 关键词：压扭性构造 ; compresso-shear structure ; 板内构造 ; intraplate tectonics ; 西北地区 ; Northwest China
• 页码：p.105-111
• 图表：6 illus., 1 table, 22 refs.
• 分类号：0300
• issnNo：ISSN1001-1552
• isbnNo：CN44-1595/P

During the late Hercynian to early Indosinian, most of main oceanic basins of Chinese continent were closed and then had been folded into mountains. The final assembly of different terrenes forms the whole continental plate and the Meso-Cenozoic range-basin system. By studying the settlement motion trajectory and modes of different prototype basins or depressions, and the tectonic movement recorded in strata, and the formation and evolution of the structure, and the evidence of the evolution and transformation of the late time, the authors probe into the kinematics process of basin-range coupling system and its constraining on the structural deformation system, in order to reveal the dynamics mechanisms and dynamical conversion of basin-range coupling system in West China.