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What is Thermodynamic Stability of Carbonatites about?
The document discusses the thermodynamic analysis of secondary mineral stability in altered carbonatites from the Oldoinyo Lengai volcano in Tanzania. It highlights the dissolution of primary minerals like gregoryite and nyerereite and their replacement by low-temperature secondary minerals such as nahcolite and calcite, influenced by factors like pH and CO2 fugacity. The findings emphasize the unique mineral assemblages formed in these carbonatites under atmospheric conditions, contributing to the understa
- Author
- JHON JAIRO RAMOS FLOREZ
- Language
- EN