Progressive Interaction between Dry and Wet Mantle during High-temperature Diapiric Upwelling: Constraints from Cenozoic Kita-Matsuura Intraplate Basalt Province, Northwestern Kyushu, Japan-Reference-Cited by-同舟云学术

Progressive Interaction between Dry and Wet Mantle during High-temperature Diapiric Upwelling: Constraints from Cenozoic Kita-Matsuura Intraplate Basalt Province, Northwestern Kyushu, Japan

Published:2014-05-30 Issue:6 Volume:55 Page:1083-1128
ISSN:0022-3530
Container-title:Journal of Petrology
language:en
Short-container-title:Journal of Petrology

Author:

Sakuyama T.,Nakai S.,Yoshikawa M.,Shibata T.,Ozawa K.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/55/6/1083/4370644/egu020.pdf

Reference140 articles.

1. Element transport by dehydration of subducted sediments: Implication for arc and ocean island magmatism

2. Hydrothermal alteration of upper oceanic crust formed at a fast-spreading ridge: mineral, chemical, and isotopic evidence from ODP Site 801

3. Compositional variation of olivine-chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotites

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