1993Annual Review of Earth and Planetary SciencesRequires access

Oxygen Isotopes in Meteorites

Robert N. Clayton

Open publisher page 642 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

About this research paper

What this paper is about

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

Why it matters

OpenAlex reports 642 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

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: Meteorite, Astrobiology, Isotopes of oxygen, Oxygen, Isotope, Radiochemistry, Chemistry, Geology

Related papers

Back to paper searchBrowse research topicsOriginal source
Oxygen Isotopes in Meteorites — Research Paper | ScholarLens