Lithium abundance and isotope systematics of forearc serpentinites, Conical Seamount, Mariana forearc: Insights into the mechanics of slab-mantle exchange during subduction

Author:

Benton Laurie D.12,Ryan Jeffrey G.13,Savov Ivan P.3

Affiliation:

1. Department of Terrestrial Magnetism; Carnegie Institution of Washington; 5241 Broad Branch Road, NW, Washington D.C. 20015 USA

2. Exponent Environmental Group; 15375 30th Place, Suite 250, Bellevue Washington 98007 USA

3. Department of Geology; University of South Florida; 4202 East Fowler Avenue, Tampa Florida 33620-5201 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference64 articles.

1. Implications of a two-component marble-cake mantle;Allègre;Nature,1986

2. Petrology of young Pacific seamounts;Batiza;J. Geophys. Res.,1984

3. Benton , L. D. 1997 Origin and evolution of serpentine seamount fluids, Mariana and Izu-Bonin forearcs: Implications for the recycling of subducted material Univ. of Tulsa Tulsa, Okla

4. Lithium isotope systematics of the Marianas revisited;Benton;Goldschmidt J. Conf. Abstr.,2000

5. Boron isotope systematics of slab fluids as inferred from a serpentinite seamount, Mariana forearc;Benton;Earth Planet. Sci. Lett.,2001

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