On the origin of one basin-multiple mountain couplings in the mesozoic-cenozoic basin-range area in eastern North China
文献类型：期刊论文
| 作者 | Niu, SY; Shao, J; Hou, QL; Wang, BD; Xu, CS |
| 刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
 |
| 出版日期 | 2004 |
| 卷号 | 78期号:1页码:302-312 |
| 关键词 | Basin-mountain Coupling Mantle Plume Mantle-branch Structure Down-faulted Basin Orogenic Belt North China |
| ISSN号 | 1000-9515 |
| 文献子类 | Article |
| 英文摘要 | The basin-range coupling relation is a leading subject of the modem geology. In geometry, relations of this type include couplings between stretched orogenic belt and down-faulted basin, compressional orogenic belt and foreland basin, strike-slip orogenic belt and strike-slip basin and so on. Fault chains are the key for these couplings and there are typical examples for all these cases. The North China down-faulted basin is coupled west with the Taihang uplift, east with the Jiao-Liao Mountains, north with the Yanshan orogenic belt and south with the Dabie orogenic belt, that is to say, the central down-faulted basin and the surrounding orogenic belts bear a coupling relation within a uniform dynamistic system. Study shows that the central down-faulted basin and the North China mantle sub-plume structure have a close relation during their formation. Owing to intensive mantle sub-plume uplifting, the bottom of the lithosphere suffered from resistance, which caused the lithosphere of the eastern North China to be heated, thinned and fault-depressed. Meanwhile, mantle rocks that were detached outwards in the shape of mushroom was dissected by surrounding ductile shearing zones, which lead to decompression and unloading to generate hypomagmas, and a series of mantle-branch structures were formed around the down-faulted basin. There is an obvious comparability among these mantle branch structures (orogenic belts), and they have basin-range coupling relations with the central down-faulted basins. |
| WOS关键词 | LITHOSPHERE |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000221717300038 |
| 出版者 | GEOLOGICAL SOC CHINA |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/64678]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Niu, SY |
| 作者单位 | 1.Shijiazhuang Univ Econ, Shijiazhuang 050031, Hebei, Peoples R China 2.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Niu, SY,Shao, J,Hou, QL,et al. On the origin of one basin-multiple mountain couplings in the mesozoic-cenozoic basin-range area in eastern North China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2004,78(1):302-312. |
| APA | Niu, SY,Shao, J,Hou, QL,Wang, BD,&Xu, CS.(2004).On the origin of one basin-multiple mountain couplings in the mesozoic-cenozoic basin-range area in eastern North China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,78(1),302-312. |
| MLA | Niu, SY,et al."On the origin of one basin-multiple mountain couplings in the mesozoic-cenozoic basin-range area in eastern North China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 78.1(2004):302-312. |
入库方式： OAI收割
来源：地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。