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• W2462641567 abstract "Crustal-scale shear/suture zones hold prime importance because they are one of the critical parameters used for paleogeographic configurations of supercontinental assemblies. The Kumta suture, located on the western margin of peninsular India, has been interpreted as the eastern extension of the Betsimisaraka suture zone of Madagascar. This suture separates the Karwar block (ca. 3200 Ma tonalite-trondhjemite-granodiorite (TTG) and amphibolite) in the west from a quartzite-dominated shelf that overlies ca. 2571 Ma quartzo-feldspathic gneisses of the Dharwar block in the east. The NW/SE-trending Bondla ultramafic-mafic complex, situated in the arc just west of the Kumta suture, comprises gabbro, troctolite, wehrlite, dunite, peridotite, pyroxenite, chromitite and chromian spinel-bearing serpentinite. In this paper, we study the chemistry of Cr-spinels in chromitites and serpentinites to help understand their paleo-tectonic environments. The Cr-spinel in Bondla chromitites and serpentinites shows variations in Cr# [Cr/(Cr + Al)] ranging from 0.54 to 0.58 and 0.56 to 0.64 respectively; also, the Mg# [Mg/(Mg + Fe)] varies from 0.56 to 0.67 and 0.41 to 0.63 respectively. The Cr-spinels in serpentinites have strong chemical zoning with distinctive ferrian chromite rims (Mg# 0.41–0.63), whereas the Cr-spinels in chromitites are generally homogeneous with only occasional weak zoning. The spinel-core crystallization temperature in the serpentinite is estimated to be above 600 °C (the spinel stability field was calculated for equilibrium with Fo90 olivine), which suggests the core composition is chemically unaltered. The Cr-spinels in all studied samples have low-Al2O3 (15–23 wt%) and moderate to high-Cr# (0.54–0.69), suggesting derivation from a supra-subduction zone arc setting. The chemistry of clinopyroxene in serpentinite indicates a wide range of crystallization temperatures from 969 °C to 1241 °C at 1.0 GPa. The calculated parental magma composition was similar to that of a modern primitive tholeiitic basalt formed by a high-degree of mantle melting. We ascribe the formation of the subduction-generated Bondla arc to the closure of the ocean that led to the formation of the Kumta suture. Thus, chromian spinel chemistry proves to be a viable indicator that helps understand the thermal conditions and tectonic derivation of the Bondla ultramafic-mafic complex against a suture zone in western India." @default.
• W2462641567 created "2016-07-22" @default.
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• W2462641567 date "2016-11-01" @default.
• W2462641567 modified "2023-09-29" @default.
• W2462641567 title "Petrogenesis and tectonic setting of the Bondla mafic-ultramafic complex, western India: Inferences from chromian spinel chemistry" @default.
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• W2462641567 cites W1966685022 @default.
• W2462641567 cites W1967784536 @default.
• W2462641567 cites W1975468902 @default.
• W2462641567 cites W1976562261 @default.
• W2462641567 cites W1983377213 @default.
• W2462641567 cites W1985295636 @default.
• W2462641567 cites W1987768108 @default.
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• W2462641567 cites W1992356046 @default.
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• W2462641567 cites W2004918923 @default.
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• W2462641567 cites W2013697025 @default.
• W2462641567 cites W2017538830 @default.
• W2462641567 cites W2017649324 @default.
• W2462641567 cites W2019738508 @default.
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• W2462641567 cites W2039535921 @default.
• W2462641567 cites W2040892664 @default.
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• W2462641567 cites W2056009939 @default.
• W2462641567 cites W2056013467 @default.
• W2462641567 cites W2062237458 @default.
• W2462641567 cites W2063205632 @default.
• W2462641567 cites W2072902273 @default.
• W2462641567 cites W2080198117 @default.
• W2462641567 cites W2086086366 @default.
• W2462641567 cites W2086250167 @default.
• W2462641567 cites W2087078696 @default.
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• W2462641567 doi "https://doi.org/10.1016/j.jseaes.2016.07.004" @default.
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