Continuous Gradations among Primary Carbonatitic, Kimberlitic, Melilititic, Basaltic, Picritic, and Komatiitic Melts in Equilibrium with Garnet Lherzolite at 3

Continuous Gradations among Primary Carbonatitic, Kimberlitic, Melilititic, Basaltic, Picritic, and Komatiitic Melts in Equilibrium with Garnet Lherzolite at 3–8 GPa

Published:2005-03-18 Issue:8 Volume:46 Page:1645-1659
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

GUDFINNSSON GUDMUNDUR H.,PRESNALL DEAN C.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/46/8/1645/4500419/egi029.pdf

Reference47 articles.

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2. Barker, D. S. (1989). Field relations of carbonatites. In: Bell, K. (ed.) Carbonatites: Genesis and Evolution. London: Unwin Hyman, pp. 38–69.

3. Bohlen, S. R. & Boettcher, A. L. (1982). The quartz + coesite transformation: a precise determination and the effects of other components. Journal of Geophysical Research87, 7073–7078.

4. Brey, G. (1978). Origin of olivine melilitites—chemical and experimental constraints. Journal of Volcanology and Geothermal Research3, 61–88.

5. Brey, G. & Green, D. H. (1977). Systematic study of liquidus phase relations in olivine melilitite + H2O + CO2 at high pressures and petrogenesis of an olivine melilitite magma. Contributions to Mineralogy and Petrology61, 141–162.

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