Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

Aditi Das ¹, C. Bhattacharyya ¹

Affiliations
1 Department of Geology, University of Calcutta, 35 Ballygunge Circular Road, Kolkata - 700 019, IN

Abstract

The roughly E-W trending North Puruliya Shear Zone is characterised by generally E-W striking deformed and brecciated porphyritic granitoid gneisses, in places, along with brecciated and limonitised quartzite, aegirine-riebeckite granite gneiss and few small occurrences of apatite-magnetite rock, REE and U-Th-rich barite-bearing small pegmatites, and small bodies of alkali feldspar salite granitelsyenite and poorly exposed carbonatite at one place. The occurrence, field relation, petrography and geochemistry of the carbonatite, apatite-magnetite rock, pegmatites enriched in REE, U-Th, and barite etc. and the alkaline granitoids along the North Puruliya Shear Zone, all taken together suggest possible genetic link of the alkaline granitoids with a carbonated silicate magma emplaced at depth along the rift zone.

Keywords

Alkaline granitoid, Shear Zone, Apatite-Magnetite rock, Puruliya District, West Bengal.

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Saibal Gupta ¹, Aditi Das ¹, Sudipta Goswami ², Ananda Modak ¹, Suman Mondal ¹

Affiliations
1 Department of Geology and Geophysics, I.I.T., Kharagpur, Kharagpur - 721 302, IN
2 School of Environmental Sciences, University of East Anglia Norwich, NR4 7TJ, GB

Abstract

Inverted metamorphism in the Himalayas is closely associated with the Main Central Thrust (MCT). In the western Himalayas, the Main Central Thrust conventionally separates high grade metamorphic rocks of the Higher Himalayan Crystalline Sequence (HHCS) from unmetamorphosed rocks of the Inner sedimentary Belt. In the eastern Himalayas, the Inner sedimentary Belt is absent, and the HHCS and meta-sedimentary Lesser Himalayan Sequence (LHS) apparently form a continuous Barrovian metamorphic sequence, leading to confusion about the precise location of the MCT. In this study, it is demonstrated that migmatitic gneisses of the sillimanite zone in the higher structural levels of the HHCS are multiply deformed, with two phases of penetrative fabric formation (S_1HHCS and S_2HHCS) followed by third folding event associated with a spaced, NW-SE trending, north-east dipping foliation (S_3HHCS). The underlying LHS schists (kyanite zone and lower) are also multiply deformed, with the bedding S₀ being isoclinally folded (F_1LHS), and subsequently refolded (F_2LHS and F_3LHS). The contact zone between the HHCS and LHS is characterized by ductile, top-to-the southwest shearing and stabilization of a pervasive foliation that is consistently oriented NW-SE and dips northeast. This foliation is parallel to the S_3HHCS foliation in the HHCS, and the S_2LHS in the LHS. Early lineations in the HHCS and LHS also show different dispersions across the contact shear zone, implying that pre-thrusting orientations of the two units were distinct. The contact shear zone is therefore interpreted to be a plane of structural discordance, shows a shear sense consistent with thrust movement and is associated with mineral growth during Barrovian metamorphism. It may well be considered to represent the MCT in this region.

Keywords

Inverted Metamorphism, Main Central Thrust, Higher Himalayan Crystalline Sequence, North Sikkim.

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