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学科主题: Geosciences, Multidisciplinary
题名: Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change
作者: Clift, PD
通讯作者: p.clift@abdn.ac.uk
刊名: GEOPHYSICAL RESEARCH LETTERS
发表日期: 2010
卷: 37, 页:#NAME
收录类别: sci
部门归属: [Clift, Peter D.] Univ Aberdeen, Sch Geosci, Kings Coll, Aberdeen AB24 3UE, Scotland; [Clift, Peter D.] Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou, Guangdong, Peoples R China
项目归属: 海洋地质
摘要: Surface erosion is the most significant process responsible for the recycling of continental crust into the upper mantle, and controls both exhumation in mountain belts and the long-term global climate via chemical weathering. Earlier studies have highlighted the importance of climate instability since the onset of Northern Hemispheric Glaciation (similar to 3 Ma) as being the primary influence causing high erosion rates since that time. Here I show that synchronous pulses of erosion and exhumation occurred across Eurasia, in North America and in Africa starting after 33 Ma, with a prominent peak around 16 Ma. Correlation of these erosional events with changes in global climate suggests that they are controlled by surface processes. Because these climate events involve both cooling and warming periods the importance of increased seasonality is emphasized as being the key factor in controlling global erosion and exhumation throughout the Cenozoic. Citation: Clift, P. D. (2010), Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change, Geophys. Res. Lett., 37, L09402, doi: 10.1029/2010GL043067.
原文出处: 查看原文
WOS记录号: WOS:000277478000004
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/4328
Appears in Collections:中科院边缘海地质重点实验室_期刊论文

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Clift, PD.Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change,GEOPHYSICAL RESEARCH LETTERS,2010,37():#NAME
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