Magma source components in an arc-continent collision zone: the Flores-Lembata sector, Sunda arc, Indonesia
- 1 October 1990
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 105 (5) , 585-601
- https://doi.org/10.1007/bf00302497
Abstract
No abstract availableKeywords
This publication has 53 references indexed in Scilit:
- Isotope geochemistry of xenoliths from East Africa: Implications for development of mantle reservoirs and their interactionPublished by Elsevier ,2002
- Quantification of Nb, Ta, Ti and V anomalies in magmas associated with subduction zones: Petrogenetic implicationsPublished by Elsevier ,2002
- Geochemistry of basaltic and gabbroic rocks from the West Mariana basin and the Mariana trenchPublished by Elsevier ,2002
- The geochemistry of marine sediments, island arc magma genesis, and crust-mantle recyclingEarth and Planetary Science Letters, 1989
- Crustal contamination versus subduction zone enrichment: Examples from the Lesser Antilles and implications for mantle source compositions of island arc volcanic rocksGeochimica et Cosmochimica Acta, 1987
- The Lead, Neodymium and Strontium Isotopic Structure of Ocean Ridge BasaltsJournal of Petrology, 1982
- “Kerguelen: Continental fragment or oceanic island?”: Petrology and isotopic geochemistry evidenceEarth and Planetary Science Letters, 1979
- Seismic refraction and reflection studies of crustal structure of the Eastern Sunda and Western Banda ArcsJournal of Geophysical Research, 1977
- Petrology of the leucite‐bearing lavas in New South Wales∗Journal of the Geological Society of Australia, 1973
- Isotopic and chemical constraints on models of magma genesis in volcanic arcsEarth and Planetary Science Letters, 1971