Origin of Fe–Ni–Cu (Co) sulfide and Fe–Ti oxide minerals in the c. 1.77 Ga dolerite dyke, Singhbhum Craton (eastern India)
- 6 October 2021
- journal article
- Published by Geological Society of London in Geological Society, London, Special Publications
- Vol. 518 (1), 553-574
- https://doi.org/10.1144/sp518-2021-46
Abstract
Dolerite dyke swarms are widespread within the Singhbhum Craton (eastern India) that emplaced from the Neoarchean to Paleoproterozoic era just after the stabilization of crust before c. 3 Ga. These dyke swarms are oriented in NE–SW to NNE–SSW, NW–SE to WNW–ESE, east–west and north–south directions. The WNW–ESE-trending c. 1.77 Ga Pipilia dyke swarm is sampled from the Satkosia area of Orissa state. The dyke shows a noticeable disparity in terms of the modal proportion and grain size of pyroxenes, plagioclase, Fe–Ti oxide minerals and texture across the trend. In places the primary silicates are altered to secondary hydrated mineral assemblages of amphibole, chlorite and sericite. The primary silicates are clinopyroxene (augite – Mg# = 65.7–82.6; En37–48Fs11–17Wo36–41), orthopyroxene (clinoenstatite – Mg# = 68.5–78; En63–70Fs20–29Wo4–5) and plagioclase (An11–39Ab44–82Or1–7) and the Fe–Ti oxides are titanomagnetite (FeO, 34.38–39.50 wt%; Fe2O3, 48.26–56.21 wt%; TiO2, 5.05–9.60 wt%) and ilmenite (FeO, 40.75–43.79 wt%; Fe2O3, 3.54–10.03 wt%; TiO2, 47.82–50.87 wt%). Application of two-pyroxene thermometry yields an equilibration temperature range of 1065–978°C, and coexisting titanomagnetite–ilmenite pairs reveal 731.39–573.37°C under the oxygen fugacity (fO2) condition NNO + 0.3 to FMQ − 1.03. The dyke contains disseminated sulfides at the interstices of Fe–Ti oxides and silicates. Major sulfide minerals are pyrite, chalcopyrite and vaesite; pyrite–vaesite assemblages occur in association with secondary silicate minerals. Pyrite grains contain variable concentrations of Co (0.01–5.70 wt%) and Ni (0.02–1.95 wt%). Coexisting vaesite contains Co (2.42–10.44 wt%), Ni (26.40–47.88 wt%) and Fe (7.32–26.55 wt%). Texture, sulfide–silicate assemblage and the presence of low metal/S sulfides such as the pyrite–vaesite assemblage indicate that primary Fe–Ni sulfides (pyrrhotite–pentlandite) that segregated from immiscible sulfide liquid at high temperature are modified by late magmatic/hydrothermal fluid activities. Numerous sulfide-bearing deposits hosted in ultramafic–mafic intrusions of Paleoproterozoic age have been recorded globally and the occurrence of Fe–Ni sulfides in the c. 1.77 Ga Pipilia dyke swarm in the Singhbhum Craton enhances the exploration potential of this craton in eastern India.This publication has 63 references indexed in Scilit:
- The Emeishan large igneous province: A synthesisGeoscience Frontiers, 2014
- Siberian Traps large igneous province: Evidence for two flood basalt pulses around the Permo-Triassic boundary and in the Middle Triassic, and contemporaneous granitic magmatismEarth-Science Reviews, 2013
- PGE geochemistry of low-Ti high-Mg siliceous mafic rocks within the Archaean Central Indian Bastar Craton: implications for magma fractionationTschermaks Mineralogische und Petrographische Mitteilungen, 2010
- Two independent processes responsible for compositional zonation in mafic dykes of the Åland-Åboland Dyke Swarm, Kestiö Island, SW FinlandLithos, 2009
- Dating the Oldest Greenstone in India: A 3.51-Ga Precise U-Pb SHRIMP Zircon Age for Dacitic Lava of the Southern Iron Ore Group, Singhbhum CratonThe Journal of Geology, 2008
- Ore Deposits of the Platinum-Group ElementsElements, 2008
- The genesis of Archaean chromitites from the Nuasahi and Sukinda massifs in the Singhbhum Craton, IndiaPrecambrian Research, 2006
- Geochemistry and petrogenesis of Neoarchaean high-Mg low-Ti mafic igneous rocks in an intracratonic setting, Central India craton: Evidence for boninite magmatismGEOCHEMICAL JOURNAL, 2006
- Geochemistry of late Mesozoic adakites from the Sulu belt, eastern China: magma genesis and implications for crustal recycling beneath continental collisional orogensGeological Magazine, 2005
- Platinum-group minerals from the Nuasahi ultramafic-mafic complex, Orissa, IndiaMineralogical Magazine, 1997