Dmisteinbergite, CaAl<sub>2</sub>Si<sub>2</sub>O<sub>8</sub>, a Metastable Polymorph of Anorthite: Crystal-Structure and Raman Spectroscopic Study of the Holotype Specimen

Dmisteinbergite, CaAl<sub>2</sub>Si<sub>2</sub>O<sub>8</sub>, a Metastable Polymorph of Anorthite: Crystal-Structure and Raman Spectroscopic Study of the Holotype Specimen

The crystal structure of dmisteinbergite has been determined using crystals from the type locality in Kopeisk city, Chelyabinsk area, Southern Urals, Russia. The mineral is trigonal, with the following structure: <i>P</i>312, <i>a</i> = 5.1123(2), <i>c</i> = 14.74...

Full description

Bibliographic Details
Main Authors: Andrey A. Zolotarev, Sergey V. Krivovichev, Taras L. Panikorovskii, Vladislav V. Gurzhiy, Vladimir N. Bocharov, Mikhail A. Rassomakhin
Format: Article
Language:English
Published: MDPI AG 2019-09-01
Series:Minerals
Subjects:
dmisteinbergite
feldspar
polymorphism
metastability
burned coal dumps
Kopeisk
Ural region
crystal structure
Raman spectroscopy
Online Access:https://www.mdpi.com/2075-163X/9/10/570

Internet

https://www.mdpi.com/2075-163X/9/10/570

Similar Items