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

4Citations
Citations of this article
19Readers
Mendeley users who have this article in their library.

Abstract

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 on 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. Copyright © 2008 by The Geochemical Society of Japan.

Cite

CITATION STYLE

APA

Kaneoka, I. (2008). On the degassing state and the chemical structure of the Earth’s interior inferred from noble gas isotopes - Past and recent views. Geochemical Journal. The Physiological Society of Japan. https://doi.org/10.2343/geochemj.42.3

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free