Recycled metasomatized lithosphere as the origin of the Enriched Mantle II (EM2) end-member: Evidence from the Samoan Volcanic Chain-Reference-Cited by-同舟云学术

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Recycled metasomatized lithosphere as the origin of the Enriched Mantle II (EM2) end-member: Evidence from the Samoan Volcanic Chain

Published:2004-04 Issue:4 Volume:5 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Workman R. K.¹,Hart S. R.¹,Jackson M.¹,Regelous M.,Farley K. A.²,Blusztajn J.¹,Kurz M.¹,Staudigel H.³

Affiliation:

1. Woods Hole Oceanographic Institution; 266 Woods Hole Road,; Woods Hole; Massachusetts; 02543; USA

2. Geological and Planetary Sciences Division; California Institute of Technology; Pasadena; California; 91125; USA

3. Scripps Institution of Oceanography; University of California, San Diego; La Jolla; California; 92093; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference140 articles.

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

3. Stable isotopic composition of upper oceanic crust formed at a fast spreading ridge, ODP Site 801;Alt;Geochem. Geophys. Geosyst.,2003

4. A model for the evolution of strontium and lead isotopes in a dynamic Earth;Armstrong;Rev. Geophys.,1968

5. Trace element modeling of aqueous fluid - peridotite interaction in the mantle wedge of subduction zones;Ayers;Contrib. Mineral. Petrol.,1998

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