This study was financially supported by the National Natural Science Foundation of China (No. 40672024) and the Knowledge Innovation Project of the Chinese Academy of Sciences (No. KJCX2-SW-N20, KJCX2-SW-N03).
This study was financially supported by the National Natural Science Foundation of China (No. 40672024) and the Knowledge Innovation Project of the Chinese Academy of Sciences (No. KJCX2-SW-N20, KJCX2-SW-N03).
Abstract: In-situ high-pressure energy dispersive X-ray diffraction experiments of malachite have been performed using diamond anvil cell and synchrotron radiation. The highest recorded pressure is up to 17.4 GPa. The experimental results reveal that malachite experienced two phase transitions at 0.7 and 7.8 GPa, and the last one is reversible.
Abstract: In-situ high-pressure energy dispersive X-ray diffraction experiments of malachite have been performed using diamond anvil cell and synchrotron radiation. The highest recorded pressure is up to 17.4 GPa. The experimental results reveal that malachite experienced two phase transitions at 0.7 and 7.8 GPa, and the last one is reversible.
LIU Yingxin, QIN Shan, LI Haijian, LI Xiaodong, LI Yanchun, LIU Jing.2009. High-Pressure Behavior of Copper Carbonate: Data from Malachite[J]. ACTA GEOLOGICA SINICA(English edition),83(3):615~617
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