Инд. авторы: Sagatova D., Shatskiy A.F., Sagatov N.E., Gavryushkin P.N., Litasov K.D.
Заглавие: Calcium orthocarbonate, Ca2CO4-Pnma: A potential host for subducting carbon in the transition zone and lower mantle
Библ. ссылка: Sagatova D., Shatskiy A.F., Sagatov N.E., Gavryushkin P.N., Litasov K.D. Calcium orthocarbonate, Ca2CO4-Pnma: A potential host for subducting carbon in the transition zone and lower mantle // Lithos. - 2020. - Vol.370. - Art.105637. - ISSN 0024-4937. - EISSN 1872-6143.
Внешние системы: DOI: 10.1016/j.lithos.2020.105637; WoS: 000558896300023;
Реферат: eng: A novel structure of calcium orthocarbonate Ca2CO4-Pnma has been discovered using ab-initio crystal structure prediction methods (AIRSS and USPEX) based on the density functional theory. This phase appears above 13 GPa and remains stable to at least 50 GPa and 2000 K according to the calculations within quasi-harmonic approximation. Thus, the discovered phase can be stable at Earth's transition zone and lower mantle P-T conditions. The carbon atoms in the discovered phase are presented in 4-fold coordination, and its structure is similar to the high-pressure and high-temperature alpha(H)'-Ca2SiO4 phase. (C) 2020 Elsevier B.V. All rights reserved.
Ключевые слова: MINERALOGY; POLYMORPHS; CACO3; BRAZIL; ARAGONITE; PHASE; Otthocarbonate; INCLUSIONS; AB-INITIO; HIGH-PRESSURE; Density functional theory; Subduction; Lower mantle; Transitions zone; DIAMOND; Ca2CO4;
Издано: 2020
Физ. характеристика: 105637