Multiple growth of zirconolite in marble (Mogok metamorphic belt, Myanmar): evidence for episodes of fluid metasomatism and Zr–Ti–U mineralization in metacarbonate systems

<p>Fluid infiltration into (meta-)carbonate rocks is an important petrologic process that induces metamorphic decarbonation and potential mineralization of metals or nonmetals. The determination of the infiltration time and the compositional features of reactive fluids is essential to understa...

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Bibliographic Details
Main Authors: Q. Guo, S. Guo, Y. Yang, Q. Mao, J. Yuan, S. Wu, X. Liu, K. Sein
Format: Article
Language:English
Published: Copernicus Publications 2024-01-01
Series:European Journal of Mineralogy
Online Access:https://ejm.copernicus.org/articles/36/11/2024/ejm-36-11-2024.pdf