Disordered rhombohedral K<sub>2</sub>Ca<sub>2</sub>(CO<sub>3</sub>)<sub>3</sub>: a supposedly transient state within an ambiguous transformation route on decompression

Author(s)
Ronald Miletich, S. Miloš, P. Lotti, A. Likhacheva, A. Romanenko, S. Rashchenko, A. Shatskiy
Abstract

Within the K2CO3-CaCO3 system on P,T variation relevant to the Earth's geotherm [1], trigonal K2Ca2(CO3)3 is one of the known solid key phases with an apparent stability under the conditions of formation. Early descriptions report on intensive polysynthetic twinning in morphologically trigonal crystals [2], and the structure was later solved according to acentric R3 space-group symmetry, but with a model proposed by Winbo et al. (1997) [3] showing conspicuous ADP's and bond lengths.

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
Università degli Studi di Milano, Siberian Branch of the Russian Academy of Sciences, Russian Academy of Sciences
Journal
Acta Crystallographica. Section A: Foundation and Advances
Volume
2024
No. of pages
1
ISSN
0108-7673
DOI
https://doi.org/10.1107/s205327332409750x
Publication date
08-2024
Peer reviewed
Yes
Austrian Fields of Science 2012
105113 Crystallography, 105116 Mineralogy
Portal url
https://ucrisportal.univie.ac.at/en/publications/3bf125ea-c4dd-46f8-a15c-ffbc0a9e1be2