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...
Main Authors: | Corgne, A, Keshav, S, Wood, B, McDonough, W, Fei, Y |
---|---|
Format: | Journal article |
Sprog: | English |
Udgivet: |
2008
|
Lignende værker
-
New metal-silicate partition coefficients and constraints on core composition and oxygen fugacity during Earth accretion
af: Corgne, A, et al.
Udgivet: (2007) -
Accretion and core formation: constraints from metal-silicate partitioning.
af: Wood, B
Udgivet: (2008) -
Reconciling metal–silicate partitioning and late accretion in the Earth
af: Terry-Ann Suer, et al.
Udgivet: (2021-05-01) -
The dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melt
af: Zervas, Deborah A
Udgivet: (2010) -
Constraints on oxygen fugacity within metal capsules
af: Berry, Andrew, et al.
Udgivet: (2018)