Breakdown of residual zircon in the Izu arc subducting slab during backarc rifting

Author:

Hirai Yasuhiro123,Yoshida Takanori1,Okamura Satoshi1,Tamura Yoshihiko3,Sakamoto Izumi4,Shinjo Ryuichi5

Affiliation:

1. Sapporo Campus, Hokkaido Education University, Sapporo, Hokkaido 002-8502, Japan

2. Division of Natural System, Kanazawa University, Kanazawa, Ishikawa 920-1192, Japan

3. Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa 237-0061, Japan

4. Department of Marine and Earth Sciences, Tokai University, Shimizu, Shizuoka 424-0902, Japan

5. Department of Physics and Earth Sciences, University of the Ryukyus, Okinawa 903-0213, Japan

Publisher

Geological Society of America

Subject

Geology

Reference35 articles.

1. Element transport from slab to volcanic front at the Mariana arc: Journal of Geophysical Research;Elliott;Solid Earth,1997

2. Thorium isotope evidence for melting of the mafic oceanic crust beneath the Izu arc;Freymuth;Geochimica et Cosmochimica Acta,2016

3. Petrology and geochemistry of lavas from the Sumisu and Torishima backarc rifts;Fryer;Earth and Planetary Science Letters,1990

4. Orogenic Andesites and Plate Tectonics;Gill,1981

5. Petrology and geochemistry of Pliocene-Pleistocene volcanic rocks from the Izu Arc;Gill,1992

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