Chemical and isotopic diversity in basalts dredged from the East Pacific Rise at 10°S, the fossil Galapagos Rise and the Nazca plate

Author:

Batiza Rodey,Oestrike Richard,Futa Kiyoto

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference37 articles.

1. Isotopic and chemical effects produced in a continuously differentiating convective earth mantle;Allegre;Philos. Trans. R. Soc. London,1980

2. The origin and petrology of young oceanic central volcanoes: Are most tholeiitic rather than alkalic?;Batiza;Geology,1980

3. Trace element and isotopic evidence for magma mixing in transitional and alkalic basalts from the East Pacific Rise at 8°N;Batiza,1980

4. Easter volcanic chain (southeast Pacific): A mantle hot line;Bonatti;J. Geophys. Res.,1977

5. Estimation of the depth of origin of basic magmas: A modified thermodynamic approach and a comparison with experimental melting studies;DePaolo;Contrib. Mineral. Petrol.,1979

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