1. Geochemistry and C–O and Nd–Sr isotope characteristics of the 2.4 Ga Hogenakkal carbonatites from the South Indian Granulite Terrane: evidence for an end-Archaean depleted component and mantle heterogeneity.
- Author
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Pandit, M. K., Kumar, M., Sial, A. N., Sukumaran, G. B., Piementle, Marcio, and Ferreira, V. P.
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GRANULITE , *DISPLACED terranes , *CARBONATITES , *CRUST of the earth - Abstract
The South Indian Granulite Terrane (SGT) is a collage of Archaean to Neoproterozoic age granulite facies blocks that are sutured by an anastomosing network of large-scale shear systems. Besides several Neoproterozoic carbonatite complexes emplaced within the Archaean granulites, there are also smaller Paleoproterozoic (2.4 Ga, Hogenakkal) carbonatite intrusions within two NE-trending pyroxenite dikes. The Hogenakkal carbonatites, further discriminated into sövite and silicate sövite, have high Sr and Ba contents and extreme light rare earth element (LREE) enrichment with steep slopes typical of carbonatites. The C- and O-isotopic ratios [δ13CVPDB = −6.7 to −5.8‰ and δ18OVSMOW = 7.5–8.7‰ except a single18O-enriched sample (δ18O = 20.0‰)] represent unmodified mantle compositions. TheεNd values indicate two groupings for the Hogenakkal carbonatites; most samples show positiveεNd values, close to CHUR (εNd = −0.35 to 2.94) and named high-εNd group while the low-εNd group samples show negative values (−5.69 to −8.86), corresponding to depleted and enriched source components, respectively. The87Sr/86Sriratios of the two groups also can be distinguished: the high-εNd ones have low87Sr/86Sriratios (0.70161–0.70244) while the low-εNd group shows higher ratios (0.70247–0.70319). We consider the Nd–Sr ratios as primary and infer derivation from a heterogeneous mantle source. The emplacement of the Hogenakkal carbonatites may be related to Paleoproterozoic plume induced large-scale rifting and fracturing related to initiation of break-up of the Neoarchean supercontinent Kenorland. [ABSTRACT FROM PUBLISHER]
- Published
- 2016
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