Oxygen isotope composition of carbonates, silicates, and oxides in selected carbonatites: constraints on crystallization temperatures of carbonatite magmas

Author:

Haynes Elizabeth A,Moecher David P,Spicuzza Michael J

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference56 articles.

1. Secondary processes in carbonatites: petrology of ‘rødberg’ (hematite–calcite–dolomite carbonatite) of the Fen complex, Telemark (South Norway);Andersen;Lithos,1984

2. Temperature–HF fugacity trends during crystallization of calcite carbonatite magma in the Fen complex, Norway;Andersen;Min. Mag.,1991

3. Oxygen isotope fractionations involving diopside, forsterite, magnetite, and calcite: application to geothermometry;Chiba;Geochim. Cosmochim. Acta,1989

4. Coghlan, R.A.N., 1990. Studies of diffusional transport: grain boundary transport of oxygen in feldspars, diffusion of oxygen, strontium, and the REEs in garnet, and thermal histories of granitic intrusions in south-central Maine using oxygen isotopes. PhD thesis, Brown University.

5. 18O/16O and 13C/12C ratios of coexisting minerals in the Oka and Magnet Cove carbonatite bodies;Conway;J. Geol.,1969

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