Geochemistry of Evaporitic Lacustrine Deposits
1980/05/01 by Hans P. Eugster, H P Eugster · 1 citation
Earth and Planetary Sciences · Engineering · #Hydrocarbon exploration and reservoir analysis #Paleontology and Stratigraphy of Fossils
paper · doi:10.1146/annurev.ea.08.050180.000343
openalex publication_date 1980/05/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/25
Abstract
Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-rich parental melts that are mostly mantle derived. They dominantly consist of carbonate minerals such as calcite, dolomite, and ankerite, as well as minor ...Read More
Cited by
Related
- Carbonatites: Classification, Sources, Evolution, and Emplacement
- Calcite-saturated natrocarbonatites: composition, crystal morphology, and weathering
- Metasomatic ijolite, glimmerite, silicocarbonatite, and antiskarn formation: carbonatite and silicate phase equilibria in the system Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O–O2–CO2
- Carbonate build-ups in lacustrine, hydrothermal and fluvial settings: comparing depositional geometry, fabric types and geochemical signature
- Non-alkali metals titrate silica out of carbonatite melts into insoluble silicate minerals