Sound velocity of CaSiO<sub>3</sub> perovskite suggests the presence of basaltic crust in the Earth's lower mantle.

Sound velocity of CaSiO₃ perovskite suggests the presence of basaltic crust in the Earth's lower mantle.

Gréaux, Steeve; Irifune, Tetsuo; Higo, Yuji; Tange, Yoshinori; Arimoto, Takeshi; Liu, Zhaodong; Yamada, Akihiro.

Gréaux S; Geodynamics Research Center, Ehime University, Matsuyama, Japan. greaux@sci.ehime-u.ac.jp.
Irifune T; Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo, Japan. greaux@sci.ehime-u.ac.jp.
Higo Y; Geodynamics Research Center, Ehime University, Matsuyama, Japan.
Tange Y; Earth-Life Science Institute, Tokyo Institute of Technology, Tokyo, Japan.
Arimoto T; Japan Synchrotron Radiation Research Institute, SPring-8, Hyogo, Japan.
Liu Z; Japan Synchrotron Radiation Research Institute, SPring-8, Hyogo, Japan.
Yamada A; Geodynamics Research Center, Ehime University, Matsuyama, Japan.

Nature ; 565(7738): 218-221, 2019 01.

Article en En | MEDLINE | ID: mdl-30626940

Texto completo: 1 Banco de datos: MEDLINE Idioma: En Año: 2019 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Idioma: En Año: 2019 Tipo del documento: Article