Experimental evidence of fast transport of trace elements in planetary basaltic crusts by high temperature metamorphism-Reference-Cited by-同舟云学术

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Experimental evidence of fast transport of trace elements in planetary basaltic crusts by high temperature metamorphism

Published:2013-04 Issue: Volume:368 Page:101-109
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Yamaguchi A.,Mikouchi T.,Ito M.,Shirai N.,Barrat J.A.,Messenger S.,Ebihara M.

Funder

Grant-in-Aid for Scientific Research from Ministry of Education, Science, and Technology, Japan, NIPR Research Project Funds, KP-6

NASA Origins Program Grant

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference32 articles.

1. Abundance of the elements: meteoritic and solar;Anders;Geochim. Cosmochim. Acta,1989

2. The Stannern trend eucrites: contamination of Main-Group eucritic magmas by crustal partial melts;Barrat;Geochim. Cosmochim. Acta,2007

3. Relative chronology of crust formation on asteroid Vesta: insights from the geochemistry of diogenites;Barrat;Geochim. Cosmochim. Acta,2010

4. Shock metamorphism as a fundamental process in the evolution of planetary bodies: information from meteorites;Bischoff;Eur. J. Mineral.,1992

5. REE diffusion in feldspar;Cherniak;Chem. Geol.,2002

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