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Late Quaternary downcutting rates of the Qianyou river from U/Th speleothem Dates, Qinling mountains, China

Published online by Cambridge University Press:  20 January 2017

Wang Fei ,
Li Hongchun ,
Zhu Rixiang  and
Qin Feizhou
Wang Fei*
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Li Hongchun
Affiliation:
Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, USA
Zhu Rixiang
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Qin Feizhou
Affiliation:
Department of Physics and Information, University of Ningxia, Yinchuan 750021, China
*
*Corresponding author. Fax: +86 10 62010846. E-mail address:[email protected](F. Wang).
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Abstract

Dating deposits in caves formed by rivers may yield insight into rates and processes of bedrock incision. Three cave passages at different levels have developed in the walls of the Qianyou River valley in the Qinling mountains, south of the city of Xian, China. Twelve speleothem samples near the position of palaeowater tables in three cave passages are dated by the 230Th dating method. The results show that the river cut down at the rate of 0.23 ± 0.02 mm/yr from 358,000 ± 38,000 to 247,000 ± 28,000 yr ago, 0.19 ± 0.03 mm/yr from 247,000 ± 28,000 to 118,000 ± 19,000 yr ago, and 0.51 ± 0.08 mm/yr from 118,000 ± 19,000 yr ago until today. These fall very close to the glacial–interglacial transition following marine oxygen isotope stages 10, 8, and 6, respectively. The increase in downcutting rates during the interglacial period is consistent with warm, wet weather, increasing rates of erosion. This may lead us toward an underlying mechanism for modulating incision that is not in a direct response to the presence of headwater glaciers.

Keywords

Qianyou RiverSpeleothemQinling mountains, China
Type
Research Article
Information
Quaternary Research , Volume 62 , Issue 2 , September 2004 , pp. 194 - 200
Copyright
University of Washington

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