长江第一湾附近构造作用下的河流地貌演化

doi:10.11867/j.issn.1001-8166.2017.05.0488

地球科学进展 ›› 2017, Vol. 32 ›› Issue (5): 488 -501. doi: 10.11867/j.issn.1001-8166.2017.05.0488

所属专题：青藏高原研究——青藏科考；

长江第一湾附近构造作用下的河流地貌演化

陶亚玲 ^1, ²(

), 常宏 ^1, ^*(

)

1.中国科学院地球环境研究所,陕西西安 710075
2.中国科学院大学,北京 100049

收稿日期:2017-01-10 修回日期:2017-03-10 出版日期:2017-05-20
通讯作者: 常宏 E-mail:taoyl@ieecas.cn;changh@loess.llqg.ac.cn
基金资助:
国家自然科学基金重大项目“渐新世以来亚洲内陆干旱化与西风气候演化”(编号:41290250)资助

River Geomorphic Evolution Connected to Tectonics Around the First Bend of Yangtze River

Yaling Tao ^1, ²( ), Hong Chang ^1, ^*( )

1.Institute of Earth Environment,Chinese Academy of Sciences,Xi’an 710075, China
2.University of Chinese Academy of Sciences,Beijing 100049, China

Received:2017-01-10 Revised:2017-03-10 Online:2017-05-20 Published:2017-05-20
Contact: Hong Chang E-mail:taoyl@ieecas.cn;changh@loess.llqg.ac.cn
About author:
First author:Tao Yaling (1988-), female,Jingchuan County, Gansu Province, Master student. Research areas include tectonic geomorphology and fluvial geomorphology.E-mail:taoyl@ieecas.cn
Supported by:
Project supported by the National Natural Science Foundation of China “Asia interior aridification and westerlies evolution since the Oligocene”(No.41290250)

全文 ( 29 ) 下载PDF ( 932 )

长江第一湾的成因及时间是长江水系和青藏高原东南缘构造作用及水系发育演化史上的重要科学问题,受到国内外众多学者的关注。关于第一湾的形成有袭夺说和非袭夺说2种观点,且分歧一直持续至今。长江的东西贯通经历了漫长的地质过程,这段历史的重建,需要时间和空间上可靠地质证据和年代数据的印证与约束。随着近年来越来越多的方法用于研究长江发育演化过程,使得时空上和不同方法间的对比研究成为了可能。

关键词: 长江第一湾, 金沙江, 河流重组与袭夺, 沉积物, 年龄约束

The origin and formation time of the first bend are important scientific problems in the Yangtze River system and the evolution of the river system, even tectonic research around the southeastern margin of the Qinghai-Tibet Plateau. These problems have attracted the attention of many domestic and international scholars and they hold two different opinions. one is river capture hypothesis; another hypothesis is river natural adaptation to terrain. It is necessary to get reliable geological evidences and chronological data in order to reconstruct the evolution history of the Yangtze River. In the recent years, much work has been done to study the evolution history of the Yangtze River. Thus, it is possible now to integrate all the relevant chronological data and geological evidences to understand the evolution of Yangtze River.

Key words: The First Bend, Jinsha River, Reorganization and capture of drainage lines, Sediments, Age constraints.

中图分类号:

P931.1

图1 青藏东南缘构造地质简图(修改自参考文献[15])

Fig.1 The geological map of southeastern Tibet (modified after reference[15])

图2 青藏高原东南缘主要河流示意图

Fig.2 The main rivers originated from southeastern Tibet

图3 长江第一湾附近的断层展布及地貌形态示意图

Fig.3 The topography and distribution of main fault nearby the first bend

图4 长江流域及重要地貌单元示意图

Fig.4 The Yangtze River Basin and the important geomorphologic unit

图5 金沙江流域研究中发现的湖盆沉积物示意图

Fig.5 Lacustrine sediments in the Jinsha River Basin

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