Return to search

Deformation of a partially molten D” layer by small-scale convection and the resulting seismic anisotropy and ultralow velocity zone

No description available.
Identiferoai:union.ndltd.org:NAGOYA/oai:ir.nul.nagoya-u.ac.jp:2237/13018
Date11 1900
CreatorsOkamoto, Tatsuto, Sumita, Ikuro, Nakakuki, Tomoeki, Yoshida, Shigeo
PublisherElsevier
Source SetsNagoya University
Languageen_US
Detected LanguageEnglish
TypeArticle(author)

Page generated in 0.0018 seconds