Magma flux rates are fundamental for global geochemical cycles.
New meteorites and improved geochemical techniques have recently identified several different parent bodies for basalt (eucrite, angrite) and ~peridotite (ureilite, pallasite)
Speaker: Laure Gauthiez-Putallaz
Speaker: Suzette Timmerman
Determining temporal variations in the nature and timing of diamond formation is an important step in understanding the workings of the Earth’s deep carbon cycle.
The North Qaidam Ultra-High Pressure (UHP) metamorphic belt is located at the North margin of Tibetan Plateau, NW China.