Genesis of Mariana shoshonites: Contribution of the subduction component
- 10 January 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 106 (B1) , 589-608
- https://doi.org/10.1029/2000jb900342
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- Mineral-aqueous fluid partitioning of trace elements at 900°C and 2.0 GPa: Constraints on the trace element chemistry of mantle and deep crustal fluidsPublished by Elsevier ,2000
- Oxygen Isotope Geochemistry of Oceanic-Arc LavasJournal of Petrology, 2000
- Element transport from slab to volcanic front at the Mariana arcJournal of Geophysical Research, 1997
- Experimental evidence for the origin of lead enrichment in convergent-margin magmasNature, 1995
- Mineral/matrix partition coefficients for orthopyroxene, plagioclase, and olivine in basaltic to andesitic systems: A combined analytical and experimental studyGeochimica et Cosmochimica Acta, 1994
- Isotope Geochemistry of Leg 129 Basalts: Implications for the Origin of the Widespread Cretaceous Volcanic Event in the PacificPublished by International Ocean Discovery Program (IODP) ,1992
- Evidence from Muriah, Indonesia, for the Interplay of Supra-Subduction Zone and Intraplate Processes in the Genesis of Potassic Alkaline MagmasJournal of Petrology, 1991
- Physical volcanology of the submarine Mariana and Volcano ArcsBulletin of Volcanology, 1989
- Shoshonitic volcanism in the Northern Mariana Arc: 1. Mineralogic and major and trace element characteristicsJournal of Geophysical Research, 1989
- The volcanism of southern Italy: Role of subduction and the relationship between potassic and sodic alkaline magmatismJournal of Geophysical Research, 1989