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Ca3[C2O5]2[CO3] is a pyrocarbonate which can be formed at p, T-conditions prevalent in the Earth’s transition zone

Author / Organization: Dominik Spahr, Lkhamsuren Bayarjargal, Maxim Bykov, Lukas Brüning, Pascal L. Jurzick, Yu Wang, Victor Milman, Keith Refson, Mohamed Mezouar, Björn Winkler

File Format PDF (Portable Document Format)
Publication Year 2024
Source Host HAL Open Science (hal.science)
License / Terms Open Access / Creative Commons

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