Abstract
This paper presents the results of a study of the thermal behavior of fedotovite K2Cu3O(SO4)3 and piypite K4Cu4O(SO4)4∙(Na,Cu)Cl minerals in a wide temperature range. The crystal structure of the holotype piypite specimen is refined at room temperature. The mechanisms of thermal expansion of minerals depending on the crystal structure are described.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have