Vesicularity and CO2 in mid-ocean ridge basalt

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Abstract

Vesicles and included CO2 are enriched in deep-sea basalts that are also enriched in light rare earth and incompatible elements. This enrichment probably results from a unique deep mantle origin of such melts but may have been modified by CO2 bubbles rising in shallow magma chambers.

Suggested Citation

Moore, J.G., 1979, Vesicularity and CO2 in mid-ocean ridge basalt: Nature, v. 282, no. 5736, p. 250-253, https://doi.org/10.1038/282250a0.

Publication type Article
Publication Subtype Journal Article
Title Vesicularity and CO2 in mid-ocean ridge basalt
Series title Nature
DOI 10.1038/282250a0
Volume 282
Issue 5736
Year Published 1979
Language English
Publisher Nature Publications
Contributing office(s) Volcano Science Center
Description 4 p.
First page 250
Last page 253
Additional publication details