中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Quantitatively Tracking the Elevation of the Tibetan Plateau Since the Cretaceous: Insights From Whole-Rock Sr/Y and La/Yb Ratios

文献类型:期刊论文

作者Hu, Fangyang3,4; Wu, Fuyuan1,2,4; Chapman, James B.7; Ducea, Mihai N.3,6; Ji, Weiqiang1,4; Liu, Shuwen5
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2020-08-16
卷号47期号:15页码:10
关键词paleo-elevation magmatic rocks Tibetan Plateau Cretaceous Cenozoic
ISSN号0094-8276
DOI10.1029/2020GL089202
英文摘要Crustal thickness, elevation, and Sr/Y and (La/Yb)(N) of magmatic rocks are strongly correlated for subduction-related and collision-related mountain belts. We quantitatively constrain the paleo-elevation of the Tibetan Plateau since the Cretaceous using empirically derived equations. The results are broadly consistent with previous estimates based on stable isotope and structural analyses, supporting a complex uplift history. Our data suggest that a protoplateau formed in central Tibet during the Late Cretaceous and was higher than the contemporaneous Gangdese arc. This protoplateau collapsed before the India-Asia collision, during the same time period that elevation in southern Tibet was increasing. During the India-Asia collision, northern and southern Tibet were uplifted first followed by renewed uplift in central Tibet, which suggests a more complicated uplift history than commonly believed. We contend that a broad paleovalley formed during the Paleogene in central Tibet and that the whole Tibetan Plateau reached present-day elevations during the Miocene. Plain Language Summary Paleo-elevation is an important factor in understanding the mountain building processes. Strong correlations are observed between crustal thickness, elevation, and Sr/Y and (La/Yb)(N) of magmatic rocks for both subduction-related and collision-related mountain belts. We established empirical equations derived from modern examples and applied them to constrain the paleo-elevation evolution of the Tibetan Plateau since the Cretaceous. Our calculated results are broadly consistent with previous estimates based on stable isotope and structural analyses and document a complex uplift history. In central Tibet, a proto-plateau with an elevation >3,000 m was formed during the Late Cretaceous and was higher than the Gangdese continental arc in the south. This protoplateau collapsed at the same time as the southern Tibet plateau (Lhasaplano) was uplifted prior to the India-Asia collision formed before the India-Asia collision. During the India-Asia collision in the Cenozoic, northern and southern Tibet were uplift first, followed by uplift of central Tibet. A paleovalley was formed in central Tibet during the Paleogene and elevations of the whole Tibetan Plateau similar to the present-day were achieved during the Miocene.
WOS关键词INDIA-ASIA COLLISION ; SOUTHERN TIBET ; LHASA TERRANE ; QIANGTANG TERRANE ; GANGDESE MOUNTAINS ; TECTONIC EVOLUTION ; CRUSTAL THICKNESS ; MAGMATISM ; CONSTRAINTS ; EOCENE
资助项目National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41902055] ; China Postdoctoral Science Foundation[2018M640177] ; U.S. National Science Foundation[EAR-1725002] ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project[PN-III-P4-ID-PCCF-2016-0014]
WOS研究方向Geology
语种英语
WOS记录号WOS:000560376100092
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; U.S. National Science Foundation ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project ; Romanian Executive Agency for Higher Education, Research, Development and Innovation Funding project
源URL[http://ir.iggcas.ac.cn/handle/132A11/97674]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Hu, Fangyang
作者单位1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
3.Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
5.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Beijing, Peoples R China
6.Univ Bucharest, Fac Geol & Geophys, Bucharest, Romania
7.Univ Wyoming, Dept Geol & Geophys, Laramie, WY 82071 USA
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Hu, Fangyang,Wu, Fuyuan,Chapman, James B.,et al. Quantitatively Tracking the Elevation of the Tibetan Plateau Since the Cretaceous: Insights From Whole-Rock Sr/Y and La/Yb Ratios[J]. GEOPHYSICAL RESEARCH LETTERS,2020,47(15):10.
APA Hu, Fangyang,Wu, Fuyuan,Chapman, James B.,Ducea, Mihai N.,Ji, Weiqiang,&Liu, Shuwen.(2020).Quantitatively Tracking the Elevation of the Tibetan Plateau Since the Cretaceous: Insights From Whole-Rock Sr/Y and La/Yb Ratios.GEOPHYSICAL RESEARCH LETTERS,47(15),10.
MLA Hu, Fangyang,et al."Quantitatively Tracking the Elevation of the Tibetan Plateau Since the Cretaceous: Insights From Whole-Rock Sr/Y and La/Yb Ratios".GEOPHYSICAL RESEARCH LETTERS 47.15(2020):10.

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来源:地质与地球物理研究所

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