Constraints from partitioning experiments on the composition of subduction-zone fluids
- 1 March 1996
- journal article
- Published by Springer Nature in Nature
- Vol. 380 (6571) , 237-240
- https://doi.org/10.1038/380237a0
Abstract
No abstract availableKeywords
This publication has 19 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
- Aspects of magma genesis in arcsLithos, 1994
- Destructive plate margin magmatism: Geochemistry and melt generationLithos, 1994
- Cerium/lead and lead isotope ratios in arc magmas and the enrichment of lead in the continentsNature, 1994
- Fluid-melt-rock interaction in mafic eclogites and coesite-bearing metasediments: Constraints on volatile recycling during subductionChemical Geology, 1993
- Metasomatism of the sub-arc mantle inferred from trace elements in Philippine xenolithsNature, 1992
- Physical model of source region of subduction zone volcanicsJournal of Geophysical Research, 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
- Partitioning of Cu, Sn, Mo, W, U, and Th between melt and aqueous fluid in the systems haplogranite-H2O?HCl and haplogranite-H2O?HFContributions to Mineralogy and Petrology, 1991