Partitioning of elements between peridotite and H2O at 2.0–3.0 GPa and 900–1100°C, and application to models of subduction zone processes
- 1 August 1997
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 150 (3-4) , 381-398
- https://doi.org/10.1016/s0012-821x(97)00096-4
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas: Evidence from high-pressure experiments and natural rocksPublished by Elsevier ,2003
- Chemical characteristics of island-arc basalts: Implications for mantle sourcesPublished by Elsevier ,2003
- The role of water in the petrogenesis of Mariana trough magmasPublished by Elsevier ,2002
- Rutile-aqueous fluid partitioning of Nb, Ta, Hf, Zr, U and Th: implications for high field strength element depletions in island-arc basaltsPublished by Elsevier ,2002
- Water and the solid EarthNature, 1994
- Rutile solubility and mobility in supercritical aqueous fluidsContributions to Mineralogy and Petrology, 1993
- Metasomatism of the sub-arc mantle inferred from trace elements in Philippine xenolithsNature, 1992
- Partitioning of trace elements between olivine and aqueous fluids at highP-T conditions: implications for the effect of fluid composition on trace-element transportEarth and Planetary Science Letters, 1991
- Fluid influence on the trace element compositions of subduction zone magmasPhilosophical Transactions A, 1991
- Mantle Oxidation State and Its Relationship to Tectonic Environment and Fluid SpeciationScience, 1990