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Microstructural and compositional variations of allanite in hydrothermal veins: Implications for REE mobilization in Chhotanagpur Granite Gneiss Complex, Purulia district, West Bengal, India.

Authors :
Maiti, Prithwiraj
Datta, Aparajita
Chaudhury, Trisrota
Tripathy, Sujit Kumar
Dey, Monotrisha
Khandolkar, Shilpa V
Ekka, Anjana Ritu
Source :
Journal of Earth System Science. Jun2024, Vol. 133 Issue 2, p1-29. 29p.
Publication Year :
2024

Abstract

This study employs a combination of texture and composition of allanite to investigate the chemical evolution of rare earth elements (REEs) in the hydrothermal veins within the Chhotanagpur Granite Gneiss Complex around Kalapathar area, Purulia district, West Bengal, India. Allanite occurs as pockets and lumps in the hydrothermal veins. Locally, the allanite pockets/lumps have high concentrations of REEs (∑REEs ~9.8 wt.%), Th (up to 1427.2 ppm) and U (up to 642.1 ppm). Three hydrothermal fluids and associated REE mobilization have been distinguished and characterized. The hydrothermal fluid1 causes metasomatic addition of REEs that leads to the formation of early REE-enriched allanite. Hydrothermal fluid2 imposed changes in the texture and composition of the allanite where the early allanite was replaced by relatively REE-depleted allanite following the substitution scheme REE+3 + (Fe+2, Mg+2) → Ca+2 + (Al, Fe+3). The hydrothermal fluid3 is marked by the alteration of allanites to the bastnaesite and monazite. REEs have been transported mainly in aqueous chloro-complexes with high to moderate salinity and low homogenization temperature (257°–361°C). The timing of the hydrothermal event is established through U–Th–total Pb dating of monazite, yielding at around 875 ± 43 Ma. Research highlights: The allanite clots and lumps in hydrothermal veins within CGGC around Kalapathar, Purulia District, West Bengal display high ∑REEs up to 9.8 wt.% along with Th and U up to 1427.22 and 642.14 ppm, respectively. The hydrothermal event has been characterized linked with two distinct varieties of allanite growth. The transportation of REEs occurs in aqueous chloro-complexes during the hydrothermal event. The timing of hydrothermal events and growth of the allanites has been determined. REE-enriched magmatic intrusion. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
02534126
Volume :
133
Issue :
2
Database :
Academic Search Index
Journal :
Journal of Earth System Science
Publication Type :
Academic Journal
Accession number :
176758135
Full Text :
https://doi.org/10.1007/s12040-024-02259-6