Tracing the formation and differentiation of the Earth by non-traditional stable isotopes

被引：0
|
作者：
Fangzhen Teng
Shuijiong Wang
Frédéric Moynier
机构：
[1] University of Washington,Isotope Laboratory, Department of Earth and Space Sciences
[2] China University of Geosciences,State Key Laboratory of Geological Processes and Mineral Resources
[3] Université de Paris,Institut de Physique du Globe de Paris
[4] Institut Universitaire de France,State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences
[5] China University of Geosciences,undefined
来源：
Science China Earth Sciences | 2019年 / 62卷
关键词：
Non-traditional stable isotopes; Differentiation of the Earth; Crust-mantle interactions; Atmospheric evolution; Snowball Earth; Mass extinction;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
The Earth has grown from chaotically mixed small dusts and gases to its present highly differentiated layered structure over the past 4.567 billion years. This differentiation has led to the formation of the atmosphere, hydrosphere, biosphere, crust, mantle, and core. The timing and mechanism for the formation and evolution of these different layers are still subjects of intense debate. This review brings together recent advances in using non-traditional stable isotopes to constrain major events and processes leading to the formation and differentiation of the Earth, including the Moon-forming giant impact, crust-mantle interactions, evolution of life, the rise of atmospheric oxygen, extreme paleoclimate changes, and cooling rate of magmas.
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页码：1702 / 1715
页数：13
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