Rapid Ascent of Aphyric Mantle Melts through the Overriding Crust in Subduction Zones: Evidence from Variable Uranium-Series Disequilibria, Amorphous Hydrous Alteration Microtextures in Crystal Rims, and Two-Pyroxene Pseudo-Decompression Paths

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ADS bibcode
2014AGUFM.V51A4725Z
year
2014
Listed Authors
Zellmer, G. F.
Freymuth, H.
Hsieh, H. H.
Hwang, S. L.
Iizuka, Y.
Miller, C. A.
Rubin, K. H.
Sakamoto, N.
Yurimoto, H.
Listed Institutions
Soil & Earth Sciences Group, IAE, Massey University, Palmeston North, New Zealand
School of Earth Sciences, University of Bristol, Bristol, United Kingdom
Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan
Department of Materials Science and Engineering, National Dong Hwa University, Hualien County, Taiwan
Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan
Department of Geology & Geophysics, SOEST, Univ Hawaii, Honolulu, HI, United States
Department of Geology & Geophysics, SOEST, Univ Hawaii, Honolulu, HI, United States
Division of Earth and Planetary Sciences, Hokkaido University, Sapporo, Japan
Division of Earth and Planetary Sciences, Hokkaido University, Sapporo, Japan

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