Pre-Quaternary Sea-Level Changes

A. Hallam A. Hallam
1984 Annual Review of Earth and Planetary Sciences 348 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

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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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

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DOI
10.1146/annurev.ea.12.050184.001225