Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change
Clift, PD
刊名GEOPHYSICAL RESEARCH LETTERS
2010
卷号37页码:#NAME
ISSN号0094-8276
通讯作者p.clift@abdn.ac.uk
中文摘要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.
学科主题Geosciences, Multidisciplinary
收录类别SCI
原文出处AMER GEOPHYSICAL UNION
WOS记录号WOS:000277478000004
公开日期2011-07-03
内容类型期刊论文
源URL[http://ir.scsio.ac.cn/handle/344004/4328]  
专题南海海洋研究所_中科院边缘海地质重点实验室
推荐引用方式
GB/T 7714
Clift, PD. Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change[J]. GEOPHYSICAL RESEARCH LETTERS,2010,37:#NAME.
APA Clift, PD.(2010).Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change.GEOPHYSICAL RESEARCH LETTERS,37,#NAME.
MLA Clift, PD."Enhanced global continental erosion and exhumation driven by Oligo-Miocene climate change".GEOPHYSICAL RESEARCH LETTERS 37(2010):#NAME.
个性服务
查看访问统计
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


©版权所有 ©2017 CSpace - Powered by CSpace