Peridotites and gabbros from the Parece Vela backarc basin: Unique tectonic window in an extinct backarc spreading ridge-Reference-Cited by-同舟云学术

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Peridotites and gabbros from the Parece Vela backarc basin: Unique tectonic window in an extinct backarc spreading ridge

Published:2003-07 Issue:7 Volume:4 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Ohara Yasuhiko¹,Fujioka Kantaro²,Ishii Teruaki³,Yurimoto Hisayoshi⁴

Affiliation:

1. Hydrographic and Oceanographic Department of Japan; Tokyo 104-0045 Japan

2. Japan Marine Science and Technology Center; Yokosuka 237-0061 Japan

3. Ocean Research Institute; University of Tokyo; Tokyo 164-8639 Japan

4. Department of Earth Sciences; Tokyo Institute of Technology; Tokyo 152-8551 Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Solar-system abundances of the elements;Anders;Geochim. Cosmochim. Acta,1982

2. The Mid-Atlantic Ridge near 45°N, XVI: Serpentinized ultramafic intrusions;Aumento;Can. J. Earth Sci.,1970

3. Empirical correction factors for the electron microanalysis of silicates and oxides;Bence;J. Geol.,1968

4. Origin of extensional core complexes: Evidence from the Mid-Atlantic Ridge at Atlantis Fracture Zone;Blackman;J. Geophys. Res.,1998

5. Geophys. Monogr. Ser.;Bloomer,1995

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