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Prehnite and Pumpellyite in the Archaean Sitagota Volcanics near Deori, Bhandara District, Maharashtra


Affiliations
1 Department of Earth Sciences, Indian Institute of Technology, Powai, Mumbai - 400 076, India
2 Department of Applied Geology, Indian School of Mines, Dhanbad - 826 004, India
     

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In this communication we report for the first time the occurrence and microprobe analyses of prehnite and pumpellyite in amygdules of metabasalt from Karu Pahar near Deori, Bhandara district, Maharashtra. The metabasalt belongs to the Sitagota Volcanics of the Late Archaean Khairagarh Group of the Dongargarh Supergroup. Pumpellyite occurs as fibrous aggregates, lining or filling amygdules, whereas prehnite occurs sporadically in amygdules as clusters of tiny prismatic crystals. Pumpellyite is iron-rich, between 10.3 and 13.1 wt% Fe2O3 Chlorite is found in close association with pumpellyite in a few of the amygdules. The absence of zeolite, and the presence of prehnite and pumpellyite in the Sitagota metabasalt indicate prehnite-pumpellyite facies metamorphism.

Keywords

Prehnite, Pumpellyite, Amygdule, Metabasalt, Maharashtra.
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  • Prehnite and Pumpellyite in the Archaean Sitagota Volcanics near Deori, Bhandara District, Maharashtra

Abstract Views: 222  |  PDF Views: 3

Authors

S. C. Patel
Department of Earth Sciences, Indian Institute of Technology, Powai, Mumbai - 400 076, India
D. Asthana
Department of Applied Geology, Indian School of Mines, Dhanbad - 826 004, India
C. S. Acharya
Department of Applied Geology, Indian School of Mines, Dhanbad - 826 004, India

Abstract


In this communication we report for the first time the occurrence and microprobe analyses of prehnite and pumpellyite in amygdules of metabasalt from Karu Pahar near Deori, Bhandara district, Maharashtra. The metabasalt belongs to the Sitagota Volcanics of the Late Archaean Khairagarh Group of the Dongargarh Supergroup. Pumpellyite occurs as fibrous aggregates, lining or filling amygdules, whereas prehnite occurs sporadically in amygdules as clusters of tiny prismatic crystals. Pumpellyite is iron-rich, between 10.3 and 13.1 wt% Fe2O3 Chlorite is found in close association with pumpellyite in a few of the amygdules. The absence of zeolite, and the presence of prehnite and pumpellyite in the Sitagota metabasalt indicate prehnite-pumpellyite facies metamorphism.

Keywords


Prehnite, Pumpellyite, Amygdule, Metabasalt, Maharashtra.