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
Keywords
CarbonatiteAnkeriteDolomiteGeologyGeochemistryCalciteCarbonateIgneous rockMantle (geology)MineralogyChemistrySiderite
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Publication Info
- Year
- 1984
- Type
- article
- Volume
- 12
- Issue
- 1
- Pages
- 205-243
- Citations
- 348
- Access
- Closed
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Cite This
A. Hallam
(1984).
Pre-Quaternary Sea-Level Changes.
Annual Review of Earth and Planetary Sciences
, 12
(1)
, 205-243.
https://doi.org/10.1146/annurev.ea.12.050184.001225
Identifiers
- DOI
- 10.1146/annurev.ea.12.050184.001225