Metal-silicate partitioning and constraints on core composition and oxygen fugacity during Earth accretion

We present the results of new partitioning experiments between metal and silicate melts for a series of elements normally regarded as refractory lithophile and moderately siderophile and volatile. These include Si, Ti, Ni, Cr, Mn, Ga, Nb, Ta, Cu and Zn. Our new data obtained at 3.6 and 7.7 GPa and b...

Полное описание

Библиографические подробности
Главные авторы: Corgne, A, Keshav, S, Wood, B, McDonough, W, Fei, Y
Формат: Journal article
Язык:English
Опубликовано: 2008