Geochemical characteristics of West Molokai shield- and postshield-stage lavas: Constraints on Hawaiian plume models

Author:

Xu Guangping1,Frey Frederick A.1,Clague David A.2,Abouchami Wafa,Blichert-Toft Janne3,Cousens Brian4,Weisler Marshall5

Affiliation:

1. Department of Earth, Atmospheric, and Planetary Sciences; Massachusetts Institute of Technology; Room 54-1226,; Cambridge; Massachusetts; 02139; USA

2. Monterey Bay Aquarium Research Institute; 7700 Sandholdt Road,; Moss Landing; California; 95039; USA

3. Ecole Normale Superieure de Lyon; UMR CNRS 5570; Lyon; France

4. Ottawa-Carleton Geoscience Centre, Department of Earth Sciences; Carleton University; Ottawa, Ontario; Canada; K1S 5B6

5. School of Social Science-Archaeology Program; University of Queensland; St Lucia; Queensland 4072; Australia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference108 articles.

1. Temporal evolution of Pb isotopes in shield lavas from Haleakala Volcano;Abouchami;Geophys. Res. Abstr.,2006

2. High precision lead isotope systematics of lavas from the Hawaiian Scientific Drilling Project;Abouchami;Chem. Geol.,2000

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

4. Geophys. Monogr. Ser.;Basu,1996

5. Partitioning coefficients between olivine and silicate melts;Bedard;Lithos,2005

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