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DOI10.1360/03wd0402
An important form of basin-mountain coupling: Orogenic belt and flank basin
Erchie, W
发表日期2004
ISSN1001-6538
EISSN1861-9541
起始页码632
结束页码636
卷号49期号:6
英文摘要Orogeny is always associated with the erosion and sediments carried by both transverse and longitudinal river systems. Those two river systems transport sediments into foreland or hinterland basin and flank basin. Longitudinal river systems prevail in and around the Tibetan Plateau due to the fact that they flow parallel to the strike of structures within the developing mountain belt. The flank basins surrounded the Tibetan Plateau and adjacent areas are developed in different tectonic settings, including inland, continental margin and deep ocean, most of them containing oil and natural gas. Those basins not only have longer evolution histories than foreland basins but also are more complete in their records of deposition. Coupling of orogeny and flank basin deposition also occurred widely in pre-Cenozoic time, in particular, the coupling between the Qinling orogenic belt and Songpan-Ganzi flysch flank basin is the most distinctive. The evolution of ancient latitudinal rivers derived from the Qinling orogenic belt during periods of mountain building was controlled not only by landforms but also by the lateral extrusion of the crustal fragments.
关键词RIVERCOLLISIONEVOLUTIONSYSTEMS
英文关键词basin-mountain coupling; longitudinal and transverse rivers; Qinghai-Tibet Plateau
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000220723800018
来源期刊CHINESE SCIENCE BULLETIN
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/257352
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GB/T 7714
Erchie, W. An important form of basin-mountain coupling: Orogenic belt and flank basin[J]. 中国科学院青藏高原研究所,2004,49(6).
APA Erchie, W.(2004).An important form of basin-mountain coupling: Orogenic belt and flank basin.CHINESE SCIENCE BULLETIN,49(6).
MLA Erchie, W."An important form of basin-mountain coupling: Orogenic belt and flank basin".CHINESE SCIENCE BULLETIN 49.6(2004).
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