Subduction factory processes beneath the Guguan cross-chain, Mariana Arc: no role for sediments, are serpentinites important?-Reference-Cited by-同舟云学术

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Subduction factory processes beneath the Guguan cross-chain, Mariana Arc: no role for sediments, are serpentinites important?

Published:2006-01-10 Issue:2 Volume:151 Page:202-221
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Stern Robert J.,Kohut Ed,Bloomer Sherman H.,Leybourne Matthew,Fouch Matthew,Vervoort Jeff

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-005-0055-2.pdf

Reference84 articles.

1. Allan JF, Batiza R, Lonsdale PF (1987) Petrology and chemistry of lavas from seamounts flanking the East Pacific Rise Axis, 21°N: implications concerning the mantle source composition for both Seamount and Adjacent EPR lavas. In: Keating B, Fryer P, Batiza R (eds) Seamounts, islands, and atolls, vol 43. American Geophysical Union, Geophysical Monograph, Washington, DC, pp 255–282

2. Balhaus CG, Berry RF, Green DH (1991) High presure calibration of the olivine--orthopyroxene--spinel oxygen barometer, implications for the oxidation state of the upper mantle. Contrib Mineral Petrol 107:27–40

3. Barnes SJ, Roeder PL (2001) The range of spinel compositions in terrestrial mafic and ultramafic rocks. J Petrol 42:2279–2302

4. Breddam K (2002) Kistufell: primitive melt from the Iceland mantle plume. J Petrol 43:345–373

5. BSVP (1981a) Island arc basalts. In: BSVP (ed) Basaltic volcanism on the terrestrial planets. Pergamon Press, New York, pp 193–213

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