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...
Những tác giả chính: | Corgne, A, Keshav, S, Wood, B, McDonough, W, Fei, Y |
---|---|
Định dạng: | Journal article |
Ngôn ngữ: | English |
Được phát hành: |
2008
|
Những quyển sách tương tự
-
New metal-silicate partition coefficients and constraints on core composition and oxygen fugacity during Earth accretion
Bằng: Corgne, A, et al.
Được phát hành: (2007) -
Accretion and core formation: constraints from metal-silicate partitioning.
Bằng: Wood, B
Được phát hành: (2008) -
Reconciling metal–silicate partitioning and late accretion in the Earth
Bằng: Terry-Ann Suer, et al.
Được phát hành: (2021-05-01) -
The dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melt
Bằng: Zervas, Deborah A
Được phát hành: (2010) -
Constraints on oxygen fugacity within metal capsules
Bằng: Berry, Andrew, et al.
Được phát hành: (2018)