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Please use this identifier to cite or link to this item: http://repository.iitr.ac.in/handle/123456789/6229
Title: Core-mantle differentiation in Mars
Authors: Rai N.
Van Westrenen W.
Published in: Journal of Geophysical Research E: Planets
Abstract: The physical and chemical conditions under which Martian core formation took place are not well constrained. We modeled the pressure, temperature, and oxygen fugacity conditions under which it would be possible to match the inferred depletions of moderately siderophile elements Ni, Co, W, Mo, Ga, P, and Ge in the Martian mantle, using new constraints on their metal-silicate partitioning behavior. Using literature metal-silicate partitioning data, we characterize the dependence of the metal-silicate partition coefficients (D) on the temperature, pressure, oxygen fugacity, and composition of the silicate melt and the metal using a uniform parameterization approach for each element. Our results show that it is impossible to simultaneously account for the Martian mantle depletions of moderately siderophile elements if the Martian core sulfur content exceeds 10.5 wt % at reducing conditions (1 log unit below the iron-wüstite (IW) buffer). At 10.5 wt % core S, the conditions that best satisfy Martian mantle abundances of the seven siderophile elements are a mean pressure of 13(±1) GPa at 2330 K, corresponding to the presence of a magma ocean at least 1000 km deep during Martian core formation. More oxidizing conditions than the iron-wüstite buffer as suggested by iron meteorites are inconsistent with mantle siderophile element abundances. Extension of our approach to the highly siderophile elements Ru, Pd, Re, Ir, and Pt shows that their Martian mantle abundances are orders of magnitude too high to be accounted for by metal-silicate equilibration at high pressure and high temperature in a magma ocean, requiring a "late veneer" stage after core formation. Key PointsWe study core formation conditions in MarsResults are consistent with a deep martian magma oceanA trade-off exists between core S content and fO2. ©2013. American Geophysical Union. All Rights Reserved.
Citation: Journal of Geophysical Research E: Planets (2013), 118(6): 1195-1203
URI: https://doi.org/10.1002/jgre.20093
http://repository.iitr.ac.in/handle/123456789/6229
Issue Date: 2013
Keywords: core formation
Mars
metal-silicate partitioning
siderophile
ISSN: 1480227
Author Scopus IDs: 36137863700
6602710945
Author Affiliations: Rai, N., Faculty of Earth and Life Sciences, VU University Amsterdam, 1081 HV Amsterdam, Netherlands
Van Westrenen, W., Faculty of Earth and Life Sciences, VU University Amsterdam, 1081 HV Amsterdam, Netherlands
Corresponding Author: Rai, N.; Faculty of Earth and Life Sciences, VU University Amsterdam, 1081 HV Amsterdam, Netherlands; email: n.rai@vu.nl
Appears in Collections:Journal Publications [ES]

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