Hotspot magmas can form by fractionation and contamination of mid-ocean ridge basalts
- 1 November 1985
- journal article
- Published by Springer Nature in Nature
- Vol. 318 (6042) , 145-149
- https://doi.org/10.1038/318145a0
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- The P-wave upper mantle structure beneath an active spreading centre: the Gulf of CaliforniaGeophysical Journal International, 1984
- Chemical composition of the mantleJournal of Geophysical Research, 1983
- Noble gas constraints on the layered structure of the mantleNature, 1983
- Isotopic and geochemical studies of nodules in kimberlite have implications for the lower continental crustNature, 1982
- Isotopic evolution of the mantle: the role of magma mixingEarth and Planetary Science Letters, 1982
- Enriched mantle: Nd and Sr isotopes in diopsides from kimberlite nodulesNature, 1980
- Preferential formation of the atmosphere–sialic crust system from the upper mantleNature, 1979
- Integrated Models of Basalt Petrogenesis: A Study of Quartz Tholeiites to Olivine Melilitites from South Eastern Australia Utilizing Geochemical and Experimental Petrological DataJournal of Petrology, 1978
- Nature and Development of Basalt Magma Sources Beneath Iceland and the Reykjanes RidgeJournal of Petrology, 1976
- Late Cenozoic Basaltic Volcanism and Development of the Rio Grande Depression in the Southern Rocky MountainsPublished by Geological Society of America ,1975