Lattice-preferred orientation of amphibole, chlorite, and olivine found in hydrated mantle peridotites from Bjørkedalen, southwestern Norway, and implications for seismic anisotropy-Reference-Cited by-同舟云学术

Lattice-preferred orientation of amphibole, chlorite, and olivine found in hydrated mantle peridotites from Bjørkedalen, southwestern Norway, and implications for seismic anisotropy

Published:2019-01 Issue: Volume:750 Page:137-152
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Kang Hyunsun,Jung Haemyeong

Funder

National Research Foundation of Korea

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference139 articles.

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4. Seismic anisotropy in the Izu-Bonin subduction system;Anglin;Geophys. Res. Lett.,2005

5. Characterization of spinel peridotites by olivine-spinel compositional relationships: review and interpretation;Arai;Chem. Geol.,1994

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