1983Annual Review of Earth and Planetary SciencesRequires access

THE ATMOSPHERES OF THE OUTER PLANETS

G. E. Hunt

Open publisher page 25 citations

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

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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

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Available 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

Key concepts: Carbonatite, Ankerite, Dolomite, Geochemistry, Geology, Calcite, Igneous rock, Carbonate

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