Calcite and dolomite in intrusive carbonatites. I. Textural variations

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• 作者：Anton R. Chakhmouradian ; Ekaterina P. Reguir…
• 刊名：Mineralogy and Petrology
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：110
• 期：2-3
• 页码：333-360
• 全文大小：4,233 KB
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• 作者单位：Anton R. Chakhmouradian (1)
  Ekaterina P. Reguir (1)
  Anatoly N. Zaitsev (2) (3)
  
  1. Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, R3T 2 N2, Canada
  2. Department of Mineralogy, St. Petersburg State University, St. Petersburg, 199034, Russia
  3. Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Mineralogy
  Geochemistry
  
• 出版者：Springer Wien
• ISSN：1438-1168

文摘

Carbonatites are nominally igneous rocks, whose evolution commonly involves also a variety of postmagmatic processes, including exsolution, subsolidus re-equilibration of igneous mineral assemblages with fluids of different provenance, hydrothermal crystallization, recrystallization and tectonic mobilization. Petrogenetic interpretation of carbonatites and assessment of their mineral potential are impossible without understanding the textural and compositional effects of both magmatic and postmagmatic processes on the principal constituents of these rocks. In the present work, we describe the major (micro)textural characteristics of carbonatitic calcite and dolomite in the context of magma evolution, fluid-rock interaction, or deformation, and provide information on the compositional variation of these minerals and its relation to specific evolutionary processes.