Experimental determination of trace element partitioning between garnet and silica‐rich liquid during anhydrous partial melting of MORB‐like eclogite
- 22 May 2004
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 5 (5)
- https://doi.org/10.1029/2003gc000638
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Partitioning of trace elements between crystals and meltsEarth and Planetary Science Letters, 2003
- Determination of Forty Two Major and Trace Elements in USGS and NIST SRM Glasses by Laser Ablation‐Inductively Coupled Plasma‐Mass SpectrometryGeostandards Newsletter, 2002
- Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditionsPrecambrian Research, 2002
- Rutile/melt partition coefficients for trace elements and an assessment of the influence of rutile on the trace element characteristics of subduction zone magmasGeochimica et Cosmochimica Acta, 2000
- Enhanced sensitivity in laser ablation-ICP mass spectrometry using helium-argon mixtures as aerosol carrierJournal of Analytical Atomic Spectrometry, 1999
- Major-element variability in the Hawaiian mantle plumeNature, 1996
- Prediction of crystal–melt partition coefficients from elastic moduliNature, 1994
- Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic meltsChemical Geology, 1994
- Geochemical characteristics of Koolau Volcano: Implications of intershield geochemical differences among Hawaiian volcanoesGeochimica et Cosmochimica Acta, 1994
- An experimental investigation of the partitioning of REE between garnet and liquid with reference to the role of defect equilibriaBeiträge zur Mineralogie und Petrographie, 1980