V11E:
Oceanic Arcs and the Evolution of Crust: Results from IODP Expeditions to the Izu-Ogasawara-Mariana Arc System and Other Advances from Pacific Island Arcs I
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V11E:
Oceanic Arcs and the Evolution of Crust: Results from IODP Expeditions to the Izu-Ogasawara-Mariana Arc System and Other Advances from Pacific Island Arcs I
Oceanic Arcs and the Evolution of Crust: Results from IODP Expeditions to the Izu-Ogasawara-Mariana Arc System and Other Advances from Pacific Island Arcs I
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Session ID#: 18140
Session Description:
Several expeditions to Pacific subduction systems have taken place over the past few years. Examples include the IODP Expeditions 350, 351 and 352, which explored the northern IBM (Izu-Ogasawara-Mariana) system, and the GeoPRISMS-related expeditions to the Aleutian Islands. Now is the time for early results to be presented and for discussions to occur between the scientific teams working in these diverse systems. Studies exploring petrology, geochemistry, geophysics, geochronology, and geodynamics of these regions are welcome. Also welcome are explorations of the links between oceanic island arcs and the development of continental crust.
Primary Convener: Yoshihiko Tamura, JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
Conveners: Mark K Reagan, University of Iowa, Department of Geoscience, Iowa City, IA, United States, Osamu Ishizuka, National Institute of Advanced Industrial Science and Technology, Ibaraki, Japan and Cathy Busby, University of California Davis, Earth and Planetary Sciences, Davis, CA, United States
Chairs: Mark K Reagan, University of Iowa, Department of Geoscience, Iowa City, IA, United States and Yoshihiko Tamura, JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan
OSPA Liaison: Cathy Busby, University of California Davis, Earth and Planetary Sciences, Davis, CA, United States
Index Terms:
8140 Ophiolites [TECTONOPHYSICS]
8185 Volcanic arcs [TECTONOPHYSICS]
8404 Volcanoclastic deposits [VOLCANOLOGY]
8413 Subduction zone processes [VOLCANOLOGY]
Abstracts Submitted to this Session:
Tuffaceous Mud is a Volumetrically Important Volcaniclastic Facies of Reararc Submarine Volcanism (128499)
See more of: Volcanology, Geochemistry and Petrology
