On the degassing state and the chemical structure of the Earth's interior inferred from noble gas isotopes-Past and recent views

被引:3
|
作者
Kaneoka, Ichiro [1 ]
机构
[1] Univ Tokyo, Earthquake Res Inst, Bunkyo Ku, Tokyo 1130032, Japan
关键词
Earth's interior; degassing state; noble gas isotopes; undegassed reservoir; non-convective mantle;
D O I
10.2343/geochemj.42.3
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The degassing state of the Earth's interior is one of the main issues in relation to the evolution of the Earth and has been discussed by many investigators over several decades. I outline some trials to reveal the state of degassing based on noble gas isotopes. Then, based oil noble gas isotope signatures so far obtained, I discuss models of the chemical structure of the Earth's interior which are inevitably related to the degassing state of the Earth. I propose a preferred model which suggests the possibility for the occurrence of relatively undegassed and possibly less fractionated reservoir(s) in the Earth's deep interior, which might be located in a relatively non-convective mantle.
引用
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页码:3 / 20
页数:18
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