Crystal preferred orientations of olivine, orthopyroxene, serpentine, chlorite, and amphibole, and implications for seismic anisotropy in subduction zones: a review
Crossref DOI link: https://doi.org/10.1007/s12303-017-0045-1
Published Online: 2017-12-07
Published Print: 2017-12
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Jung, Haemyeong
License valid from 2017-12-01