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Carbonatites; contrasting, complex, and controversial

Vadim S. Kamenetsky, Anna G. Doroshkevich, Holly A. L. Elliott and Anatoly N. Zaitsev
Carbonatites; contrasting, complex, and controversial
Elements (October 2021) 17 (5): 307-314

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 carbonatites and their surrounding metasomatic rocks (fenites) suggest that carbonatite 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.


ISSN: 1811-5209
Serial Title: Elements
Serial Volume: 17
Serial Issue: 5
Title: Carbonatites; contrasting, complex, and controversial
Affiliation: University of Tasmania, Sandy Bay, Tasmania, Australia
Pages: 307-314
Published: 202110
Text Language: English
Publisher: Mineralogical Society of America and Mineralogical Society of Great Britain and Ireland and Mineralogical Association of Canada and Geochemical Society and Clay Minerals Society, International
References: 30
Accession Number: 2022-015289
Categories: Isotope geochemistryIgneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
S02°45'00" - S02°45'00", E35°55'60" - E35°55'60"
Secondary Affiliation: Sobolev Institute of Geology and Mineralogy, RUS, Russian FederationUniversity of Derby, GBR, United KingdomSaint Petersburg State University, RUS, Russian Federation
Country of Publication: International
Secondary Affiliation: GeoRef, Copyright 2022, American Geosciences Institute. Abstract, copyright, Mineralogical Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 202206
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