Evolution of terraces I-III along the Anning River, western Sichuan, based on pollen records and terrace structure

This study reconstructs the long-term evolution of river terraces over large spatial scales along the Anning River, western Sichuan, and identifies external factors controlling terrace formation. Pollen record analysis and terrace structure indicate that formation of the middle section of terraces I...

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Bibliographic Details
Published in:Science China. Earth sciences Vol. 54; no. 1; pp. 127 - 135
Main Author: Cheng, JianWu
Format: Journal Article
Language:English
Published: Heidelberg SP Science China Press 2011
Springer Nature B.V
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Summary:This study reconstructs the long-term evolution of river terraces over large spatial scales along the Anning River, western Sichuan, and identifies external factors controlling terrace formation. Pollen record analysis and terrace structure indicate that formation of the middle section of terraces I-III resulted from the interaction of changing climates and uplift of the margins of the Qinghai-Tibet Plateau. The relative influence of climate and uplift in terrace formation changes in different periods. The terraces reveal multiple, gradual uplift events on the eastern Qinghai-Tibet Plateau, which is of great significance for determining uplift mechanisms across the entire plateau.
Bibliography:Anning River in western Sichuan, terrace formation, pollen, paleoclimate
11-5843/P
P618.130.2
P931.1
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:1674-7313
1869-1897
DOI:10.1007/s11430-010-4067-z