Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on
earth, and become a key region for comprehending the rheology and tectonic evolution of …

A quantitative understanding of crystallization and solidification is central to appreciating a
variety of phenomena at the interface between volcanology and petrology. Interpretation of …

Over the last few decades, significant advances in using geophysical techniques to image
the structure of magma plumbing systems have enabled the identification of zones of melt …

Electrically conductive regions in Earth's mantle have been interpreted to reflect the
presence of either silicate melt or water dissolved in olivine. On the basis of laboratory …

Parameterizations of experimental data constraining the influence of CO2 and H2O on
silicate melting, combined with experimental data on the stability of carbonatite in the upper …

The low-viscosity layer in the upper mantle, the asthenosphere, is a requirement for plate
tectonics. The seismic low velocities and the high electrical conductivities of the …

In implementing into a molecular dynamics simulation code a simple interionic potential
developed to describe the nine component system K2O–Na2O–CaO–MgO–FeO–Fe2O3 …

The Earth's uppermost asthenosphere is generally associated with low seismic wave
velocity and high electrical conductivity. The electrical conductivity anomalies observed from …

The Kangding geothermal field along the **anshuihe fault is a typical high-temperature
geothermal system with an enormous capacity for geothermal power generation. The …

The electrical properties of rocks and minerals are controlled by thermodynamic parameters
like pressure and temperature and by the chemistry of the medium in which the charge …