Making and breaking an island arc: A new perspective from the Oligocene Kyushu-Palau arc, Philippine Sea

Author:

Ishizuka Osamu,Taylor Rex N.1,Yuasa Makoto2,Ohara Yasuhiko

Affiliation:

1. School of Ocean and Earth Science; University of Southampton, National Oceanography Centre; Southampton; SO14 3ZH; UK

2. Institute of Geology and Geoinformation; Geological Survey of Japan, AIST; Central 7, 1-1-1,; Higashi, Ibaraki, Tsukuba; 305-8567; Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference97 articles.

1. The geochemical evolution of the Izu-Bonin arc system: A perspective from tephras recovered by deep-sea drilling;Bryant;Geochem. Geophys. Geosyst.,2003

2. The ophiolite problem: Is it really a problem?;Casey;Eos Trans. AGU,2009

3. Sedimentation on the Tonga forearc related to arc rifting, subduction erosion, and ridge collision: A synthesis of results from Sites 840 and 841;Clift;Proc. Ocean Drill. Program, Sci. Results,1994

4. 40Ar/39Ar and K-Ar geochronological age constraints for the inception and early evolution of the Izu-Bonin- Mariana arc system;Cosca;Isl. Arc,1998

5. The West Philippine Basin: An Eocene to early Oligocene back arc basin opened between two opposed subduction zones;Deschamps;J. Geophys. Res.,2002

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