Highly siderophile element (HSE) abundances in the mantle of Mars are due to core formation at high pressure and temperature-Reference-Cited by-同舟云学术

Highly siderophile element (HSE) abundances in the mantle of Mars are due to core formation at high pressure and temperature

Published:2015-01-06 Issue:4 Volume:50 Page:604-631
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Righter K.¹,Danielson L. R.²,Pando K. M.²,Williams J.³,Humayun M.³,Hervig R. L.⁴,Sharp T. G.⁴

Affiliation:

1. Mailcode KT; NASA Johnson Space Center; 2101 NASA Parkway Houston Texas 77058 USA

2. Jacobs Technology; JETS; NASA Johnson Space Center; 2101 NASA Parkway Houston Texas 77058 USA

3. National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Science; Florida State University; Tallahassee Florida 32310-3706 USA

4. ASU School of Earth and Space Exploration; PO Box 871404 Tempe Arizona 5287-1404 USA

Funder

National Aeronautics and Space Administration

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/maps.12393/fullpdf

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