New High‐Pressure Phase of CaCO3 at the Topmost Lower Mantle: Implication for the Deep‐Mantle Carbon Transportation

In this study, we have investigated the stability of CaCO3 at high pressures and temperatures using synchrotron X‐ray diffraction in laser‐heated diamond anvil cells. Our experimental results have shown that CaCO3 in the aragonite structure transforms into CaCO3‐VII (P21/c) at 27 GPa and 1,500 K wit...

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Bibliographic Details
Published inGeophysical research letters Vol. 45; no. 3; pp. 1355 - 1360
Main Authors Li, Xinyang, Zhang, Zhigang, Lin, Jung‐Fu, Ni, Huaiwei, Prakapenka, Vitali B., Mao, Zhu
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 16.02.2018
American Geophysical Union
Wiley
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