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• W573767514 endingPage "1289" @default.
• W573767514 startingPage "1263" @default.
• W573767514 abstract "The geological and metallogenic history of the Singhbhum Craton of eastern India is marked by several episodes of volcanism, plutonism, sedimentation and mineralization spanning from Paleoarchean to Mesoproterozoic in a dynamic tectonic milieu. Distinct signatures of this Archean-Proterozoic geodynamic process are preserved in discrete crustal provinces that constitute the Singhbhum Craton. Here we report new major, trace and PGE geochemical data from the ~ 3.4 Ga Iron Ore Group (IOG) volcanic rocks of the Jamda-Koira basin, a part of the BIF-bearing volcano-sedimentary sequences of the Noamundi-Jamda-Koira iron ore basin in the western part of Singhbhum Granite (SBG), and ~ 2.25 Ga metavolcanic rocks of Malangtoli. The IOG and Malangtoli volcanic rocks are porphyritic basalts and despite belonging to different ages, they exhibit similar mineralogical composition marked by clinopyroxene, plagioclase (present as both phenocryst and groundmass), opaques and volcanic glass (restricted to groundmass). The igneous mineralogy of these rocks has been overprinted by greenschist to lower amphibolite grade of metamorphism. The Malangtoli samples show low and high MgO compositional varieties. Immobile trace element compositions classify the IOG samples as andesite having a calc-alkaline composition, whereas the Malangtoli rocks correspond to basalt and andesite displaying a tholeiitic to calc-alkaline trend. The IOG basalts show low to moderate PGE contents marked by 26.23–68.35 ppb of ΣPGE, whereas the Malangtoli basalts display a moderate to high concentration of PGE (ΣPGE = 43.01–190.43 ppb). The studied samples have relatively enriched ΣPPGE ranging from 24.1–63.3 ppb (IOG) and 34–227.3 ppb (Malangtoli) against 2.2–4.1 ppb and 1.9–8.9 ppb ΣIPGE contents respectively. PPGE/IPGE ratios for IOG and Malangtoli samples range from 7.7–17.6 and 4.8–59.9. HFSE, REE and PGE compositions suggest a low degree (< 1 to 1%) of partial melting in the garnet lherzolite domain for the generation of IOG volcanic rocks. The parental magma of the Malangtoli basalts were generated by lower to higher degrees (3–< 10%) of mantle melting at depths corresponding to spinel to garnet lherzolite regime. Trace element (Zr/Nb, Th/Ta, Th/Nb, Ni/Cu) and PGE (Pd/Ir, Pd/Pt, Cu/Pd, Ni/Pd, Cu/Ir) ratios corroborate a sulphide saturated and PGE depleted character of IOG volcanic rocks that underwent crustal assimilation. In contrast, the high MgO Malangtoli basalts exhibit sulphide undersaturated, PGE undepleted nature devoid of crustal contamination whereas the low MgO Malangtoli basalts are sulphide saturated, PGE depleted and crustally contaminated. The IOG volcanic rocks correspond to intraoceanic arc with polygenetic crustal signatures, and show affinity towards arc-generated calc-alkaline basalts. The low- and high MgO basalts of Malangtoli are affiliated to transitional arc to rift-controlled back arc tectonic setting in a basinal environment that developed proximal to an active convergent margin." @default.
• W573767514 created "2016-06-24" @default.
• W573767514 creator A5002436821 @default.
• W573767514 creator A5025094061 @default.
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• W573767514 creator A5058553549 @default.
• W573767514 creator A5060053337 @default.
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• W573767514 creator A5087603053 @default.
• W573767514 date "2016-01-01" @default.
• W573767514 modified "2023-10-12" @default.
• W573767514 title "Major, trace and platinum group element (PGE) geochemistry of Archean Iron Ore Group and Proterozoic Malangtoli metavolcanic rocks of Singhbhum Craton, Eastern India: Inferences on mantle melting and sulphur saturation history" @default.
• W573767514 cites W1499747395 @default.
• W573767514 cites W1509335520 @default.
• W573767514 cites W1529203488 @default.
• W573767514 cites W1548900912 @default.
• W573767514 cites W1667967001 @default.
• W573767514 cites W1964865374 @default.
• W573767514 cites W1965976900 @default.
• W573767514 cites W1966081220 @default.
• W573767514 cites W1969859799 @default.
• W573767514 cites W1970033364 @default.
• W573767514 cites W1970922795 @default.
• W573767514 cites W1971912724 @default.
• W573767514 cites W1972002854 @default.
• W573767514 cites W1972365683 @default.
• W573767514 cites W1974639462 @default.
• W573767514 cites W1975757281 @default.
• W573767514 cites W1976424772 @default.
• W573767514 cites W1978185229 @default.
• W573767514 cites W1978592939 @default.
• W573767514 cites W1980951510 @default.
• W573767514 cites W1982798536 @default.
• W573767514 cites W1983846946 @default.
• W573767514 cites W1984773925 @default.
• W573767514 cites W1987275845 @default.
• W573767514 cites W1987405372 @default.
• W573767514 cites W1991687601 @default.
• W573767514 cites W1992736932 @default.
• W573767514 cites W1994501675 @default.
• W573767514 cites W1995798238 @default.
• W573767514 cites W1996988503 @default.
• W573767514 cites W1997659134 @default.
• W573767514 cites W1999448338 @default.
• W573767514 cites W2000012172 @default.
• W573767514 cites W2000270968 @default.
• W573767514 cites W2000593660 @default.
• W573767514 cites W2001111736 @default.
• W573767514 cites W2003940547 @default.
• W573767514 cites W2004789205 @default.
• W573767514 cites W2004872704 @default.
• W573767514 cites W2006288429 @default.
• W573767514 cites W2006824932 @default.
• W573767514 cites W2008717668 @default.
• W573767514 cites W2009643804 @default.
• W573767514 cites W2010722702 @default.
• W573767514 cites W2011176927 @default.
• W573767514 cites W2011190845 @default.
• W573767514 cites W2011549988 @default.
• W573767514 cites W2014832120 @default.
• W573767514 cites W2017568806 @default.
• W573767514 cites W2018799950 @default.
• W573767514 cites W2019082012 @default.
• W573767514 cites W2019780914 @default.
• W573767514 cites W2023885290 @default.
• W573767514 cites W2024762704 @default.
• W573767514 cites W2026250540 @default.
• W573767514 cites W2026780523 @default.
• W573767514 cites W2029989699 @default.
• W573767514 cites W2033300940 @default.
• W573767514 cites W2034180154 @default.
• W573767514 cites W2034321273 @default.
• W573767514 cites W2035045325 @default.
• W573767514 cites W2035595872 @default.
• W573767514 cites W2035722108 @default.
• W573767514 cites W2036016724 @default.
• W573767514 cites W2036631107 @default.
• W573767514 cites W2040272282 @default.
• W573767514 cites W2044095990 @default.
• W573767514 cites W2044646211 @default.
• W573767514 cites W2045697928 @default.
• W573767514 cites W2049708615 @default.
• W573767514 cites W2049894853 @default.
• W573767514 cites W2050649198 @default.
• W573767514 cites W2052675726 @default.
• W573767514 cites W2053050961 @default.
• W573767514 cites W2054261909 @default.
• W573767514 cites W2056159368 @default.
• W573767514 cites W2057620806 @default.
• W573767514 cites W2058254064 @default.
• W573767514 cites W2059416609 @default.
• W573767514 cites W2060963469 @default.
• W573767514 cites W2061359484 @default.
• W573767514 cites W2066695862 @default.
• W573767514 cites W2066941117 @default.
• W573767514 cites W2067498280 @default.
• W573767514 cites W2068604762 @default.

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