Archaean lode gold mineralisation in Bhitar Dari area of Gorumahisani–Badampahar greenstone belt, Singhbhum Craton, eastern India

[1]  A. Hofmann,et al.  The Archaean geological history of the Singhbhum Craton, India – a proposal for a consistent framework of craton evolution , 2022, Earth-Science Reviews.

[2]  A. Adhikari,et al.  Petrogenesis of the Mesoarchean (~3.05 Ga) mafic volcanics from the western Iron Ore Group volcano-sedimentary succession, Singhbhum craton, eastern India: Constraints from geochemical modelling and Sm-Nd geochronology , 2022, Lithos.

[3]  Sahendra Singh,et al.  A holistic approach on the gold metallogeny of the Singhbhum crustal province: Implications from tectono-metamorphic events during the Archean-Proterozoic regime , 2021, Precambrian Research.

[4]  A. Hofmann,et al.  3.51 Ga old felsic volcanic rocks and carbonaceous cherts from the Gorumahisani Greenstone Belt – Insights into the Palaeoarchaean record of the Singhbhum Craton, India , 2021, Precambrian Research.

[5]  A. Banerjee,et al.  Tectonic evolution of the Paleoarchean to Mesoarchean Badampahar-Gorumahisani belt, Singhbhum craton, India – Implications for coexisting arc and plume signatures in a granite-greenstone terrain , 2021 .

[6]  M. Santosh,et al.  Mantle heterogeneity and crust-mantle interaction in the Singhbhum craton, India: New evidence from 3340 Ma komatiites , 2020 .

[7]  A. Boyce,et al.  Source of gold in Neoarchean orogenic-type deposits in the North Atlantic Craton, Greenland: Insights for a proto-source of gold in sub-seafloor hydrothermal arsenopyrite in the Mesoarchean , 2020, Precambrian Research.

[8]  S. Dey,et al.  Building the core of a Paleoarchean continent: Evidence from granitoids of Singhbhum Craton, eastern India , 2019 .

[9]  D. Groves,et al.  A holistic model for the origin of orogenic gold deposits and its implications for exploration , 2019, Mineralium Deposita.

[10]  S. Reddy,et al.  Evolution of the Singhbhum Craton and supracrustal provinces from age, isotopic and chemical constraints , 2019, Earth-Science Reviews.

[11]  T. Nägler,et al.  Genesis of the Singhbhum Craton, eastern India; implications for Archean crust-mantle evolution of the Earth , 2019, Chemical Geology.

[12]  Dunyi Liu,et al.  Evidence of Enriched, Hadean Mantle Reservoir from 4.2-4.0 Ga zircon xenocrysts from Paleoarchean TTGs of the Singhbhum Craton, Eastern India , 2018, Scientific Reports.

[13]  S. Dey,et al.  Generation and evolution of Palaeoarchaean continental crust in the central part of the Singhbhum craton, eastern India , 2017 .

[14]  A. S. Venkatesh,et al.  Constraints of mineralogical characterization of gold ore: Implication for genesis, controls and evolution of gold from Kundarkocha gold deposit, eastern India , 2015 .

[15]  W. Altermann,et al.  Geochemical and ion-microprobe U–Pb zircon constraints on the Archaean evolution of Singhbhum Craton, eastern India , 2014 .

[16]  A. S. Venkatesh,et al.  ‘Indicator’ carbonaceous phyllite/graphitic schist in the Archean Kundarkocha gold deposit, Singhbhum orogenic belt, eastern India: Implications for gold mineralization vis-a-vis organic matter , 2014, Journal of Earth System Science.

[17]  D. Upadhyay,et al.  Magmatic and metamorphic history of Paleoarchean tonalite–trondhjemite–granodiorite (TTG) suite from the Singhbhum craton, eastern India , 2014 .

[18]  G. Ghosh,et al.  A 3.51 Ga bimodal volcanics‐BIF‐ultramafic succession from Singhbhum Craton: implications for Palaeoarchaean geodynamic processes from the oldest greenstone succession of the Indian subcontinent , 2012 .

[19]  M. Bose Precambrian mafic magmatism in the Singhbhum craton, eastern India , 2009 .

[20]  G. Ghosh,et al.  Reappraisal of the structure of the Western Iron Ore Group, Singhbhum craton, eastern India: Implications for the exploration of BIF-hosted iron ore deposits , 2007 .

[21]  G. N. Phillips,et al.  Link between gold provinces , 1993 .

[22]  G. Hanson,et al.  Geochemistry and Petrogenesis of Amphibolites, Kolar Schist Belt, South India: Evidence for Komatiitic Magma Derived by Low Percentages of Melting of the Mantle , 1985 .