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Late Quaternary fluvial terraces near the Daocheng Ice Cap, eastern Tibetan Plateau

Published online by Cambridge University Press:  20 January 2017

Liubing Xu  and
Shangzhe Zhou
Liubing Xu*
Affiliation:
Department of Geography, South China Normal University, Guangzhou 510631, China
Shangzhe Zhou
Affiliation:
Department of Geography, South China Normal University, Guangzhou 510631, China
*
*Corresponding author. Fax: + 86 20 85215910. E-mail address:[email protected] (L. Xu).
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Abstract

The timing of terrace formation relative to the glacial–interglacial cycle and what factors control that timing, such as changes in climate and/or uplift, are controversial. Here we present a study of the terraces along the Yazheku River using electron spin resonance (ESR) dating and analysis of the sedimentary characteristics in order to establish the timing of terrace formation and to assess the forcing mechanisms that have been proposed. The Yazheku River flows in glacial trough leading from the Haizi Shan, on the eastern Tibetan Plateau. The range was uplifted during the Quaternary and repeatedly glaciated by ice caps. The four highest major terraces (T5, T4, T3, and T2) are the result of both climatic and tectonic influences. Strath terraces T5–T2 were created during Haizi Shan glacial expansions during MIS 16, 12, 6 and 3–4, respectively. The major aggradation phases of the four terraces occurred during the deglaciations at the ends of MIS 16, 12, 6, and 2. Down-cutting, which led to the generation of the four terraces, immediately followed the deposition of the T5–T2 gravel units. These incisions occurred during the transitions between MIS 16–15, MIS 12–11, MIS 6–5, and MIS 2–1.

Keywords

Fluvial terraceGlaciationTectonic upliftClimate changeHaizi ShanEastern Tibetan Plateau
Type
Articles
Information
Quaternary Research , Volume 81 , Issue 3 , May 2014 , pp. 452 - 463
Copyright
University of Washington

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