CCPortal
DOI10.1038/s41467-021-24422-z
Mariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly
Yao J.; Cawood P.A.; Zhao G.; Han Y.; Xia X.; Liu Q.; Wang P.
发表日期2021
ISSN2041-1723
卷号12期号:1
英文摘要Initiation of Mariana-type oceanic subduction zones requires rheologically strong oceanic lithosphere, which developed through secular cooling of Earth’s mantle. Here, we report a 518 Ma Mariana-type subduction initiation ophiolite from northern Tibet, which, along with compilation of similar ophiolites through Earth history, argues for the establishment of the modern plate tectonic regime by the early Cambrian. The ophiolite was formed during the subduction initiation of the Proto-Tethys Ocean that coincided with slab roll-back along the southern and western Gondwana margins at ca. 530-520 Ma. This global tectonic re-organization and the establishment of modern plate tectonic regime was likely controlled by secular cooling of the Earth, and facilitated by enhanced lubrication of subduction zones by sediments derived from widespread surface erosion of the extensive mountain ranges formed during Gondwana assembly. This time also corresponds to extreme events recorded in climate and surface proxies that herald formation of the contemporary Earth. © 2021, The Author(s).
语种英语
scopus关键词isotope; mineral; zirconium; climate change; Gondwana; ophiolite; slab; subduction zone; tectonic rotation; Article; chemical composition; climate; conceptual model; cooling; erosion; lithosphere; Lower Cambrian; lubrication; Mesoproterozoic; ophiolite; Paleozoic; sea; sediment; stratigraphy; temperature; Tibet; water content; Brazil; China; Mariana; Minas Gerais; Xizang; Tethys
来源期刊Nature Communications
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/251394
作者单位State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi’an, 710069, China; School of Earth, Atmosphere & Environment, Monash University, Melbourne, VIC 3800, Australia; Department of Earth Sciences, The University of Hong Kong, Hong Kong, Pokfulam Road, Hong Kong; State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China
推荐引用方式
GB/T 7714
Yao J.,Cawood P.A.,Zhao G.,et al. Mariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly[J],2021,12(1).
APA Yao J..,Cawood P.A..,Zhao G..,Han Y..,Xia X..,...&Wang P..(2021).Mariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly.Nature Communications,12(1).
MLA Yao J.,et al."Mariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly".Nature Communications 12.1(2021).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Yao J.]的文章
[Cawood P.A.]的文章
[Zhao G.]的文章
百度学术
百度学术中相似的文章
[Yao J.]的文章
[Cawood P.A.]的文章
[Zhao G.]的文章
必应学术
必应学术中相似的文章
[Yao J.]的文章
[Cawood P.A.]的文章
[Zhao G.]的文章
相关权益政策
暂无数据
收藏/分享

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。