Towards a consensus on the pressure and composition dependence of sound velocity in the liquid Fe–S system
Year: 2016
Type: article
Institutions: The University of Tokyo, Tohoku University, The University of Osaka, Frontier Research Institute for Interdisciplinary Sciences, Tohoku University, Japan Synchrotron Radiation Research Institute, Tokyo Institute of Technology, High Energy Accelerator Research Organization, Institute of Materials Structure Science
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: closed
Awards: Technical development of sound velocity and density measurements of liquid iron alloys up to Martian core conditions, Chemical composition of the lower mantle and differentiation of the early Earth, 鉱物中の水素位置で読み解くマントルダイナミクス：鉱物物性の結晶化学的理解に向けて, Sound velocity and density measurements of solid iron alloys under high-pressure and high-temperature conditions, Volcanic activity and deep structure of volcanoes, Development of a pressure scale for the experiments of geofuluid in the Earth's interior, Developments of elastic velocity measurement technique with synchrotron X-ray and ultrasonic method under lowermost the mantle conditions, G6494066735, Composition and dynamics of Mercury and Mars cores approached from physical properties under high pressures, G6995474590, Density and viscosity measurements of silicate melts under lower mantle conditions, 初期地球内部における炭素分布とダイナミクスの解明
OpenAlex ID: W2467781775