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

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K. Righter, L. R. Danielson, K. M. Pando, J. Williams, M. Humayun, R. L. Hervig and T. G. Sharp

Meteoritics & Planetary Science. doi: 10.1111/maps.12393

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