Carbonatites: Contrasting, Complex, and Controversial

Author:

Kamenetsky Vadim S.12,Doroshkevich Anna G.3,Elliott Holly A. L.4,Zaitsev Anatoly N.56

Affiliation:

1. University of Tasmania, Sandy Bay, TAS, 7001, Australia

2. Fersman Mineralogical Museum, Moscow 119071, Russia

3. Sobolev Institute of Geology and Mineralogy, Novosibirsk 630090, Russia

4. Environmental Sciences, University of Derby, Derby, DE22 1GB, UK

5. Department of Mineralogy, St. Petersburg State University, St. Petersburg 199034, Russia

6. Imaging and Analysis Centre, Department of Earth Sciences, Natural History Museum, London, SW7 5BD, UK

Abstract

Carbonatites are unique, enigmatic, and controversial rocks directly sourced from, or evolved from, mantle melts. Mineral proportions and chemical compositions of carbonatites are highly variable and depend on a wide range of processes: melt generation, liquid immiscibility, fractional crystallization, and post-magmatic alteration. Observations of plutonic carbon-atites and their surrounding metasomatic rocks (fenites) suggest that carbon-atite intrusions and volcanic rocks do not fully represent the true compositions of the parental carbonatite melts and fluids. Carbonatites are enriched in rare elements, such as niobium and rare earths, and may host deposits of these elements. Carbonatites are also important for understanding the carbon cycle and mantle evolution.

Publisher

Mineralogical Society of America

Subject

Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology

Reference30 articles.

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