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

Publisher： John Wiley & Sons Inc

E-ISSN： 1945-5100|50|4|604-631

ISSN： 1086-9379

Source： METEORITICS & PLANETARY SCIENCE, Vol.50, Iss.4, 2015-04, pp. : 604-631

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