The composition and distribution of the rejuvenated component across the Hawaiian plume: Hf-Nd-Sr-Pb isotope systematics of Kaula lavas and pyroxenite xenoliths

Author:

Bizimis Michael1,Salters Vincent J. M.2,Garcia Michael O.3,Norman Marc D.4

Affiliation:

1. Department of Earth and Ocean Sciences; University of South Carolina; Columbia South Carolina 29208 USA

2. National High Magnetic Field Laboratory and Department of Earth, Ocean and Atmospheric Sciences; Florida State University; Tallahassee Florida USA

3. Department of Geology and Geophysics; University of Hawaii; Honolulu Hawaii USA

4. Research School of Earth Sciences; Australian National University; Canberra ACT Australia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference120 articles.

1. Lead isotopes reveal bilateral asymmetry and vertical continuity in the Hawaiian mantle plume;Abouchami;Nature,2005

2. Abundances of the elements: Meteoritic and solar;Anders;Geochim. Cosmochim. Acta,1989

3. Spatial and temporal variability in Hawaiian hotspot volcanism induced by small-scale convection;Ballmer;Nat. Geosci.,2011

4. Origin of garnet pyroxenite xenoliths at Salt Lake crater, Oahu, Hawaii;Beeson;Mineral. Soc. Am. Spec. Pap.,1970

5. Secondary Hawaiian volcanism formed by flexural arch decompression;Bianco;Geochem. Geophys. Geosyst.,2005

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