We conduct experiment and computational simulation to study minerals at the conditions found in Earth’s deep interiors. Our group travel to national laboratories and use synchrotron x-ray diffractionand spectroscopy to characterize the structural, electronic and geological properties of rocks under high-pressure. By mimicking deep Earth environment, a set of new theories have been raised to increase margins of our understandings in deep Earth geophysics, geochemistry and geodynamics.

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我们通过实验和理论计算研究矿物在地球内部环境下的变化。通过使用国内外同步光源设施表征高压下的原子结构、电子特征和地学特性，继而发现和进展地球内部新的矿物相变和高压下新的材料性质，研究主要包括：

1. 矿物晶体学

2. 高温高压下新的化学成分和结构

3. 高压下的功能材料