Change in mantle potential temperature through Earth time: Hotspots versus Ridges純一 木村博 川畑JUNICHI KIMURAHIROSHI KAWABATA
A. Kronrod, "Determining the Temper- ature of the Earth's Continental Upper Mantle from Geochemical and Seismic Data," Geochem. Int. 44, 232- 248 (2006).Kuskov O.L., Kronrod V.A.. Determining the Temperature of the Earth's Continental Upper Mantle from Geochemical and Seismic Data //...
Earth, third planet from the Sun and the fifth largest planet in the solar system in terms of size and mass. Its single most outstanding feature is that its near-surface environments are the only places in the universe known to harbor life. Learn more ab
Atlantic Ocean, body of salt water covering about one-fifth of Earth’s surface and separating the continents of Europe and Africa to the east from those of North and South America to the west. Its name, derived from Greek mythology, means the ‘Sea of A
Modelling the rheology of MgO under Earth's mantle pressure, temperature and strain rates. Nature 2012, 481, 177-180. [CrossRef] [PubMed]Cordier, P., Amodeo, J., Carrez, P., 2012. Modelling the rheology of MgO under Earth's mantle pressure, temperature and strain rates. Nature 481, ...
Models of large-scale viscous flow in the Earth's mantle with constraints from mineral physics and surface observations Modelling the geoid has been a widely used and successful approach in constraining flow and viscosity in the Earth's mantle. However, details of the viscos... B Steinberger,AR...
Developments in high-pressure, high-temperature research and the study of the Earth's deep interior - Magnetoconvection and thermal coupling of the Earth's... Numerical calculations of finite amplitude magnetoconvection in a rotating spherical shell are used to investigate the thermal coupling of ...
Study the Interior of the Earth Using Ultrasonic Measurements: Progress and Challenges Ultrasonic velocity measurements in the laboratory on mantle minerals and phases under relevant pressure and temperature conditions provide the key element... B Li,R. Liebermann - AGU Fall Meeting Abstracts 被引量:...
The δ18O-δD relation shows that the main source is the meteoric water, together with some sedimentary water, but there are no deep magmatic water and mantle water which recharge the geothermal water in the basin. Through examining the distribution pattern of hydrogen-oxygen isotopic signatures,...
Subduction (or sagduction) of the uppermost crust in an ultrahot orogen setting brought shales and greenstones to the lower crust. Ultrahigh temperature (UHT) conditions are the result of high mantle potential temperatures and self- heating by the radioactive inventory of the subducted lithologies...