Gravitational stability of iron-rich peridotite melt at Mars’ core-mantle boundary

Gravitational stability of iron-rich peridotite melt at Mars’ core-mantle boundary

Abstract Possible existence of dense iron-rich silicate melt layer above Mars’ core is important in understanding the nature and evolution of Mars. However, gravitational stability of iron-rich silicate melt in the Mars’ interior has not been well constrained, due to experimental difficulties in mea...

Full description

Bibliographic Details
Main Authors: Yoshio Kono, Chihiro Koyama, Nozomi M. Kondo, Koji Ohara, Hideharu Kuwahara, Ryoichi Nakada, Yuki Watanabe, Hirohisa Oda, Takehiko Ishikawa
Format: Article
Language:English
Published: Nature Portfolio 2025-03-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02117-3

Internet

https://doi.org/10.1038/s43247-025-02117-3

Similar Items