Mantle deformation during opening of the Japan Sea back-arc: Insights from peridotite xenoliths, Kawashimo, southwest Japan
Author:
Funder
University of Tokyo
Japan Society for the Promotion of Science
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference81 articles.
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2. Geochemical Signatures of High T Mantle Xenoliths from Noyamadake, SW Japan: Implications from Trace Element Characteristics;Abe,2002
3. Lattice-preferred orientation and microstructure of peridotites from ODP hole 1274A (15°39’N), mid-Atlantic ridge: testing models of mantle upwelling and tectonic exhumation;Achenbach;Earth Planet. Sci. Lett.,2011
4. Characterization of spinel peridotites by olivine–spinel compositional relationships: review and interpretation;Arai;Chem. Geol.,1994
5. Insights into petrological characteristics of the lithosphere of mantle wedge beneath arcs through peridotite xenoliths: a review;Arai;J. Petrol.,2008
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1. Deformation and melt–rock interaction in the upper mantle: Insights from the layered structure of the Horoman peridotite, Japan;Tectonophysics;2024-09
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