Experimental determination of metal/silicate partition coefficients for P, Co, Ni, Cu, Ga, Ge, Mo, and W and some implications for the early evolution of the Earth
- 1 January 1989
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 53 (1) , 173-185
- https://doi.org/10.1016/0016-7037(89)90284-6
Abstract
No abstract availableThis publication has 20 references indexed in Scilit:
- The significance of Mo for the geochemistry of the upper mantleChemical Geology, 1988
- Geochemical constraints on core formation in the EarthNature, 1986
- The depletion of siderophile elements in the Earth's mantle: new evidence from molybdenum and tungstenEarth and Planetary Science Letters, 1984
- Constraints on the Moon's origin from the partitioning behaviour of tungstenNature, 1982
- Constitution of terrestrial planetsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1981
- Composition of the earth's upper mantle—I. Siderophile trace elements in ultramafic nodulesTectonophysics, 1981
- Nickel partitioning between olivine and silicate meltEarth and Planetary Science Letters, 1978
- The heating of the earth during its formationIcarus, 1978
- Activity of iron and olivine solubility in basaltic liquidsEarth and Planetary Science Letters, 1974
- Composition of the earth: Chondritic or Achondritic?Geochimica et Cosmochimica Acta, 1971