The Formation of Barite and Celestite through the Replacement of Gypsum
Barite (BaSO<sub>4</sub>) and celestite (SrSO<sub>4</sub>) are the end-members of a nearly ideal solid solution. Most of the exploitable deposits of celestite occur associated with evaporitic sediments which consist of gypsum (CaSO<sub>4</sub>·2H<sub&g...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-02-01
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Series: | Minerals |
Subjects: | |
Online Access: | https://www.mdpi.com/2075-163X/10/2/189 |