Oxygen isotope evidence against bulk recycled sediment in the mantle sources of Pitcairn Island lavas
- 1 September 1995
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 377 (6545) , 138-141
- https://doi.org/10.1038/377138a0
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Oxygen isotope fractionations involving diopside, forsterite, magnetite, and calcite: Application to geothermometryPublished by Elsevier ,2003
- Mantle plumes from ancient oceanic crustPublished by Elsevier ,2003
- The origin of ocean island basalt end-member compositions: trace element and isotopic constraintsPublished by Elsevier ,2002
- Oxygen isotope composition of mantle peridotitePublished by Elsevier ,2002
- New software models thermodynamics of magmatic systemsEos, 1994
- Oxygen isotope evidence for recycled crust in the source of EM-type ocean island basaltsNature, 1993
- Heterogeneous mantle domains: signatures, genesis and mixing chronologiesEarth and Planetary Science Letters, 1988
- Chemical GeodynamicsAnnual Review of Earth and Planetary Sciences, 1986
- Role of subducted sediment in the genesis of ocean-island basalts: Geochemical evidence from South Atlantic Ocean islandsGeology, 1986
- The oxygen and hydrogen isotope geochemistry of clay mineralsGeochimica et Cosmochimica Acta, 1970