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Experimental Mineral Physics group

The Experimental Mineral Physics group applies a high-pressure and high-temperature experimental approach mainly using a laser-heated diamond anvil cell technique, which reproduces the condition of the deep Earth in the laboratory. We can generate pressure and tempertaure of the deep mantle (e.g. 135 GPa and 4000 K) and analyse the physical and chemcial propeties of the minerals at the base of the mantle. In particular, we can measure the elastic and sound wave velocities in minerals to better constrain the composition and mineralogical models of the deep Earth.

News

Water-rich magmas are crucial for forming copper deposits

New insights into the formation of the Tibetan Plateau

From Earth to distant worlds: ETH department is now called Earth and Planetary Sciences

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