Thermal-theological structure of the lithosphere beneath two types of basins in eastern and western China
文献类型:期刊论文
作者 | Wang, LS; Li, C; Liu, FT; Li, H; Lu, HF; Liu, SW |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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出版日期 | 2000-12-01 |
卷号 | 43页码:200-207 |
关键词 | basin lithosphere thermal-theological structure geodynamics |
ISSN号 | 1006-9313 |
文献子类 | Article |
英文摘要 | After calculating thermal-theological properties of the lithosphere in the Northern Jiangsu basin, the Bohaiwan basin as well as the Jiyang depression in the east and Tarim basin in the west of China, this paper analyzes the relationship between thermal-theological structures and tectonic evolution of the two types of basins. The results show that the thermal-rheological structures of the lithosphere directly reflect the dynamic processes. Under different dynamic environments, the style of basin formation and the differences in basin evolution are closely related to the dynamic properties of the lithosphere indicated by thermal-theological structures. |
WOS关键词 | EARTHQUAKES ; CORDILLERA ; RHEOLOGY |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000167755800013 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/75878] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Wang, LS |
作者单位 | 1.Nanjing Univ, Dept Earth Sci, Nanjing 210093, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, LS,Li, C,Liu, FT,et al. Thermal-theological structure of the lithosphere beneath two types of basins in eastern and western China[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2000,43:200-207. |
APA | Wang, LS,Li, C,Liu, FT,Li, H,Lu, HF,&Liu, SW.(2000).Thermal-theological structure of the lithosphere beneath two types of basins in eastern and western China.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,43,200-207. |
MLA | Wang, LS,et al."Thermal-theological structure of the lithosphere beneath two types of basins in eastern and western China".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 43(2000):200-207. |
入库方式: OAI收割
来源:地质与地球物理研究所
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