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Updated: Jul 6, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

地球のマントルの塩素同位体成分

M Bonifacie1, N Jendrzejewski, P Agrinier

  • 1Equipe de Physico-Chimie des Fluides, Géologiques, Institut de Physique du Globe de Paris (IPGP) and Université Paris, Diderot (UPD), CNRS-INSU-Unité Mixte de Recherche (UMR) 7154, 75251 Paris Cedex 05, France. bonifaci@gps.caltech.edu

Science (New York, N.Y.)
|March 15, 2008
PubMed
まとめ

ほとんどの海洋溶岩は塩素汚染を示しており,同位体比 (デルタ37Cl) は海水または塩塩の影響を示している. 汚染されていないマントル源は,地表貯水池よりもデルタ37Cl値が著しく低い.

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