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...
Автори: | Corgne, A, Keshav, S, Wood, B, McDonough, W, Fei, Y |
---|---|
Формат: | Journal article |
Мова: | English |
Опубліковано: |
2008
|
Схожі ресурси
Схожі ресурси
-
New metal-silicate partition coefficients and constraints on core composition and oxygen fugacity during Earth accretion
за авторством: Corgne, A, та інші
Опубліковано: (2007) -
Accretion and core formation: constraints from metal-silicate partitioning.
за авторством: Wood, B
Опубліковано: (2008) -
The dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melt
за авторством: Zervas, Deborah A
Опубліковано: (2010) -
Constraints on oxygen fugacity within metal capsules
за авторством: Berry, Andrew, та інші
Опубліковано: (2018) -
Accretion and Core Formation of Earth-like Planets: Insights from Metal–Silicate Partitioning of Siderophile and Volatile Elements
за авторством: Dominik Loroch, та інші
Опубліковано: (2024-10-01)