ARIJIT PAHARI

@ngri.org.in

Research Scholar, Geochemistry Division
CSIR-National Geophysical Research Institute

ARIJIT PAHARI


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20

Scopus Publications

301

Scholar Citations

11

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13

Scholar i10-index

Scopus Publications

  • Serpentinised Dunites of the Neoarchean Shimoga Greenstone Belt, Western Dharwar Craton, India: Insights on Ni-PGE Mineralisation and Genesis
    Th. Dhanakumar Singh, C. Manikyamba, G. Harshitha, M. Lingadevaru, K. S. V. Subramanyam, Arijit Pahari
    Geological Journal, 2025
    Ultramafic rocks of the Archean greenstone belts worldwide are potential hosts for Cu‐Ni, precious metal deposits like platinum group elements (PGEs) and gold. This study highlights the geochemical evidence and genesis of Ni‐PGE mineralisation in the ultramafic rocks of Shimoga greenstone belt of the Western Dharwar Craton, India. Petrographically, the studied rocks are identified to be serpentinised dunites, while their geochemical signatures indicate komatiitic affinity. Presence of disseminated sulphides and pronounced serpentinisation in these rocks suggest a combination of Type II (disseminated sulphides) and Type IV (post‐magmatic alterations) komatiite‐related Ni–Cu‐PGE deposits. Chondritic Al2O3/TiO2 (9.65–16.38) ratios, superchondritic Gd/YbN (1.3–1.6), depleted high‐field‐strength elements (HFSEs) (Zr, Hf), enrichment of LREE over HREE and negative Nb–Ta anomalies reflect the generation of parental melts from plume‐sourced Al‐depleted komatiites with significant crustal contamination during their emplacement. The major, trace element and PGE relationships (FeO vs. MgO, Cu vs. Pd, Ni/Cu vs. Pd/Ir) infer the origin of sulphur undersaturated primary melts through moderate to higher degrees of partial melting followed by crustal assimilation that led to PGE enrichment. These observations suggest their formation from melts derived from greater depths of the upper mantle (> 400 km) at high pressure (> 10 GPa), wherein, the mantle residue retained majorite garnet. The high Ni (avg. Ni = 6511 ppm) substantiated by high Kambalda ratio ([Ni:Cr] × [Cu:Zn] = 5.6), Ni/Cr ratios (> 1) with high concentration of PGEs (avg. ∑PGE = 3078 ppb) confirm the fertile/mineralised nature of the komatiitic source and potential Ni‐PGE mineralization in the ultramafic rocks of the Shimoga greenstone belt.
  • Forearc and back-arc mantle characteristics of the mafic-ultramafic rocks of Simlipal complex, Singhbhum Craton, India
    C. Manikyamba, M. Santosh, K.S.V. Subramanyam, G. Harshitha Reddy, Jyotisankar Ray, Asima Kar, Arijit Pahari
    Lithos, 2022
  • Geochemistry of basalts in unravelling the mantle processes and crustal evolution: Insights from the greenstone belts of western Dharwar Craton
    C. Manikyamba, Arijit Pahari, M. Santosh, K.S.V. Subramanyam, G. Harshitha Reddy
    Geosystems and Geoenvironment, 2022
    Basalts are an integral part of all the greenstone belts of Dharwar Craton which played a vital role in the thermo-tectonic evolution and mantle processes during the Archean time. Here, we evaluate the basalt geochemistry from the Holenarsipur, Shimoga and Chitradurga greenstone belts of western Dharwar Craton wherein both Sargur and Dharwar Supergroups are present reflecting a gradual change in the geodynamic processes. They have overlapping petrographic and distinct geochemical characteristics with slightly fractionated chondrite normalized rare earth element patterns for the Shimoga basalts, low order negative Eu anomalies and negative Nb and Ti anomalies with a hump at Zr-Hf. The Holenarsipur basalts display nearly flat REE patterns with low LREE/HREE [(La/Yb)N = 0.26-0.97] and negative to positive Eu (Eu/Eu* = 0.93-1.05) anomalies whereas the Chitradurga basalts show flat REE patterns [(La/Yb)N = 0.92-1.28] analogous to MORB. The U-Pb zircon age of the Holenarsipur basalts indicate 3235 ± 54 Ma with multiple thermal overprints after their deposition due to Paleoproterozoic to Mesozoic dyke emplacement. The Holenarsipur and Chitradurga basalts show partial melting trend whereas the Shimoga basalts follow fractional crystallization trajectory. Nb/La (0.13-1.33) and La/Yb (0.38-6.76) ratios of all these basalts represent the derivation of their primary magma from the lithospheric mantle with a significant asthenospheric contribution reflecting on mantle recycling. Furthermore, Nb/Yb and La/Yb relationship indicates that the Holenarsipur and Chitradurga basalts are derived from N-MORB type mantle whereas Shimoga basalts are derived from slightly enriched mantle. Nb/Yb and Th/Yb relationship show back arc basin affinity for the Chitradurga basalts whereas Holenarsipur basalts endorse oceanic arc characteristics and the Shimoga basalts display continental arc affinity. These basalts follow the spinel to spinel-garnet lherzolite melting regime and the degree of melting ranges from 10-30% resembling the global counterparts. Considering the regional geology, geochemistry and geochronology of these three greenstone belts, it is proposed that the WDC experienced three different tectono-magmatic events viz. the oceanic arc, back arc basin and continental arc during the Meso-Neoarchean which played a key role in the crustal evolution of Dharwar Craton.
  • Arc-Back Arc Cohabitation and Associated Bimodal Volcanism: Evidence from Neoarchean Raichur Greenstone Belt, Eastern Dharwar Craton, India
    Arijit Pahari, C. Manikyamba
    Geochemical Treasures and Petrogenetic Processes, 2022
  • Archean Biogeochemical Cognizance from Dharwar Craton, India — A Review
    C. Manikyamba, C. S. Sindhuja, A. C. Khelen, Arijit Pahari
    Journal of the Geological Society of India, 2022
    The Banded iron formations (BIFs) and manganese formations of Chitradurga, Shimoga and Sandur greenstone belts of Dharwar craton, associated with the stromatolitic carbonates, carbonaceous phyllites and shales along with gold mineralization, are best geological entities to evaluate the Archean biogeochemical processes and transformation of a habitable Earth. The geochemical anomalies along with C, O and S isotopic signatures of stromatolitic carbonates, carbonaceous phyllites and sulphidic BIFs reflect on biogenic signatures, fluctuating Archean ocean temperatures from 25–75°C and anoxic to euxinic redox conditions. The U-Pb detrital zircon ages of these stromatolitic carbonates indicate 3.5 to 2.6 Ga whereas the carbonaceous shales indicate 3.2–2.2 Ga reflecting the transportation of organic matter to the ocean basin during the growth of stromatolitic carbonates. The gold content of carbonaceous phyllites and sulphidic BIFs indicates hydrothermal source. The O 2 produced due to stromatolitic activity has deposited Mn and Fe of the Archean oceans as BIFs and Mn formations. The biogenic matter of the stromatolites along with other siliciclastic material, gold and sulphides derived from the volcanic activity mixed and formed as carbonaceous shales in the ocean basin under euxinic conditions. The comprehensive geological, geochemical including isotopic studies on these rock types collectively indicate the interaction of lithosphere-hydrosphere-atmosphere-biosphere in the Archean oceans which paved the way for the advanced forms of life.
  • Crustal stabilization: Evidence from the geochemistry and U–Pb detrital zircon geochronology of quartzites from Simlipal Complex, Singhbhum Craton, India
    C.S. Sindhuja, Arijit Pahari, C. Manikyamba, M. Santosh, Li Tang, Jyotisankar Ray, K.S.V. Subramanyam, Madhuparna Paul, I. Gonzalez-Alvarez, P.C. Sruthi
    Geoscience Frontiers, 2022
    Cratonic stabilization was a critical crustal process during the Hadean to Archean for the formation of cratons. The understanding of how and where this process took place is significant to evaluate the architecture of continents. The Singhbhum Craton of eastern India has well preserved Precambrian volcano-sedimentary sequences. The Simlipal volcano-sedimentary complex of Singhbhum Craton consists of circular bands of mafic volcanic rocks interlayered with quartzites/ shales/phyllites. In the present study, we report petrographic and geochemical characteristics of quartzites from Simlipal Complex coupled with U–Pb ages of detrital zircons and zircon geochemistry to understand the provenance and depositional conditions and its connection with the crustal stabilization in the Singhbhum Craton. The quartzites are texturally mature with sub-angular to sub-rounded quartz grains followed by feldspars embedded in a silty matrix. Based on modal compositions and major element ratios, these quartzites are categorized as quartz arenite and sub-lithic arenites. Trace element abundances normalized to Archean Upper Continental Crust (AUCC) display positive anomalies at U, Zr, Hf and negative anomalies at Nb. REE patterns are characterized by negative Eu anomalies (Eu/Eu* = 0.47–0.97) and flat HREE suggesting felsic provenance. These quartzites show depletion of LILE, enrichment of HFSE and transition metals relative to AUCC. High weathering indices such as CIA, PIA, and ICV are suggestive of moderate to intense chemical weathering. Low trace element ratios such as Th/Cr, Th/Sc, La/Sc, La/Co and Th/Co indicate a predominantly felsic source for these rocks. The overall geochemical signatures indicate passive margin deposition for these quartzites. Detrital zircons from the Simlipal quartzites yield U–Pb ages 3156 ± 31 Ma suggesting Mesoarchean crustal heritage. The trace element geochemistry of detrital zircons suggests that the zircons are magmatic in origin and possibly derived from the 3.1 Ga anorogenic granite/granitoid provenance of Singhbhum Craton. These observations collectively indicate the Mayurbhanj Granite and Singhbhum Granite (SBG-III) provenance for these quartzites, thereby tracking the stabilization of the eastern Indian Shield/Singhbhum Craton back to Mesoarchean.
  • Geochemical Features of Bellara Trap Volcanic Rocks of Chitradurga Greenstone Belt, Western Dharwar Craton, India: Insights into MORB-BABB Association from a Neoarchean Back-Arc Basin
    Chakravadhanula Manikyamba, Sohini Ganguly, Arijit Pahari
    Journal of Earth Science, 2021
    This study presents a comprehensive account of the petrogenetic and geodynamic evolution of the Bellara Trap volcanic rocks from the Ingaldhal Formation, Chitradurga Group, western Dharwar Craton (WDC). Geochemical attributes of these rocks are consistent with two groups with distinct evolutionary trends: one comprising tholeiitic, MORB (mid-ocean ridge basalt) type basalts (BTB) and the other corresponding to calc-alkaline andesites (BTA). Basalts are essentially composed of clinopyroxene and plagioclase whereas the andesites are porphyritic with phenocrysts of plagioclase, clinopyroxene and polycrystalline quartz embedded in a groundmass of K-feldspar, quartz and opaques. Primary igneous mineralogy is overprinted by greenschist facies metamorphism resulting in chlorite-actinolite-plagioclase assemblage. The BTB samples reflect nearly flat REE patterns with weak LREE enrichment in contrast to pronounced LREE enhancement over HREE discernible for BTA. Tectonically, the BTB samples correspond to an active mid-oceanic ridge-rift setting with a MORB composition, whereas a back-arc basin (BAB) regime is corroborated for the BTA samples fractionating from back-arc basin basalts. Geochemical imprints of subduction input are more pronounced in BTA compared to BTB as mirrored by their elevated abundances of incompatible fluid mobile elements like Ba, Th, U and LREE. The BTB is endowed with an N- to E-MORB signature attributable to minor contributions from subduction-related components at the inception of a back-arc basin in the vicinity of an active subduction system. The BTA derived through differentiation of a basaltic magma with BABB (back-arc basin basalt) affinity compositionally akin to a heterogeneous source mantle carrying depleted MORB-type and enriched arc-type components inducted with progressive subduction. The BABB-type andesites and MORB-type basalts from Bellara Traps record a compositional heterogeneity of mantle in an intraoceanic arc-back arc system. Mantle processes invoke a BABB-MORB spectrum with a MORB-like endmember and an arc-like endmember associated with a juvenile back-arc basin. This study infers a Neoarchean analogue of Mariana-type back-arc rift setting proximal to the arc with a gradual transition from anhydrous to hydrous melting processes synchronized with MORB-mantle and arc-mantle interaction during initiation of a nascent back arc adjacent to the arc. The MORB-BABB compositional spectrum for the Bellara Traps conforms to a Neoarchean back-arc basin that evolved under an extensional tectonic regime associated with incipient stages of back-arc rifting and incorporation of subduction-derived components in the mantle output. This study complies with Neoarchean intraoceanic accretionary cycle plate tectonics in WDC.
  • Understanding the role of chalcophile-siderophile elements in the petrogenesis of metabasalts of Kudremukh greenstone belt, western Dharwar Craton, India: A Platinum group elements geochemical perspective
    Arijit Pahari, Th Dhanakumar Singh, C Manikyamba, K S V Subramanyam
    Journal of Earth System Science, 2021
    The Meso-Neoarchean Kudremukh greenstone belt (KGB) of Western Dharwar craton comprises predominant metabasalts associated with banded iron formations (BIFs). The metabasalts are characterized by moderate MgO (7.23–8.97 wt.%), Ni (48–374 ppm), Cr (33–188 ppm) with a wide variation in ∑\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$$\\sum $$\\end{document}PGE (21.8–215.7 ppb) contents with 15.8–115.9 ppb Pd, 3.7–105.2 ppb Pt and 0.7–8.5 ppb Rh. Among IPGE group, Iridium, Osmium and Ruthenium range from 0.2–5.9, 1.4–7 and 1.8–7.8 ppb, respectively. These metabasalts are relatively enriched in ∑\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$$\\sum $$\\end{document}PPGE (21.8–215.7 ppb) than ∑\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$$\\sum $$\\end{document}IPGE contents (3.6–18.6 ppb). Their Pd/Ir (7.6–100.7) and Pd/Pt (0.8–5.5) ratios correspond to moderate to lower degree of melting. The abundance of PGEs in Kudremukh metabasalts is dominantly controlled by sulphide and chromite fractionation trend of the parent magma. Sulphur undersaturated nature of the parent magma is evidenced through the relationship of Pd vs. Cu. Further,̄ the Cu/Pd ratios of the studied volcanics (Cu/Pd = 1277–5747) is lower than primitive mantle (Cu/Pd = 7000), indicating early sulphide removal and S-undersaturation during magmatic differentiation. PGEs geochemistry of the studied rocks suggest early removal of sulphide melts followed by pronounced sulphide fractionation and the mantle melting episode is followed by metasomatism of the refractory mantle wedge by the fluids/melts derived from the subducting slab in a convergent margin setting. PGE systematics on the metabasalts from Kudremukh greenstone belt, western Dharwar Craton, India. The KGB metabasalts are characterised by low- moderate degrees of partial melting and high degrees of sulphide fractionation. PGE geochemistry of the KGB metabasalts infers the early sulphur undersaturated nature of magmas. PGE systematics on the metabasalts from Kudremukh greenstone belt, western Dharwar Craton, India. The KGB metabasalts are characterised by low- moderate degrees of partial melting and high degrees of sulphide fractionation. PGE geochemistry of the KGB metabasalts infers the early sulphur undersaturated nature of magmas.
  • Corrigendum: “Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining crustal accretion processes in a Neoarchean subduction-collision orogeny” (Precambrian Research (2021) 355, (S0301926821000073), (10.1016/j.precamres.2021.106097))
    C. Manikyamba, Sohini Ganguly, M. Santosh, Li Tang, C.S. Sindhuja, Arijit Pahari, Th. Dhanakumar Singh, Abhishek Saha
    Precambrian Research, 2021
  • Metallogenesis and depositional environment of the Archean-Proterozoic carbonaceous phyllites from the Dharwar Craton, India
    C.S. Sindhuja, C. Manikyamba, Arijit Pahari, M. Santosh, Li Tang
    Ore Geology Reviews, 2021
  • Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining crustal accretion processes in a Neoarchean subduction-collision orogeny
    C. Manikyamba, Sohini Ganguly, M. Santosh, Li Tang, C.S. Sindhuja, Arijit Pahari, Th. Dhanakumar Singh, Abhishek Saha
    Precambrian Research, 2021
  • Gold, uranium, thorium, and rare earth mineralization in the Kadiri Volcanic Province of Eastern Dharwar Craton, India: An evaluation of mineralogical, textural, and geochemical attributes
    Chakravadhanula Manikyamba, Naresh C Ghose, Sohini Ganguly, Arijit Pahari, Challa Satyasri Sindhuja
    Geological Journal, 2021
  • Subduction–collision processes and crustal growth in eastern Dharwar Craton: Evidence from petrochemical studies of Hyderabad granites
    Arijit Pahari, P Prasanth, Devleena M Tiwari, C Manikyamba, K S V Subramanyam
    Journal of Earth System Science, 2020
  • Mesoarchean gabbro-anorthosite complex from Singhbhum Craton, India
    C. Manikyamba, Arijit Pahari, M. Santosh, Jyotisankar Ray, C.S. Sindhuja, K.S.V. Subramanyam, Mutum Rajanikanta Singh
    Lithos, 2020
  • Geochemistry of banded sulphidic cherts of Sandur greenstone belt, Dharwar Craton, India: Constraints on hydrothermal processes and gold mineralization
    C.S. Sindhuja, C. Manikyamba, Arijit Pahari, M. Satyanarayanan
    Ore Geology Reviews, 2020
  • Evolution of geodynamic processes in Neoarchean Kadiri greenstone belt, eastern Dharwar Craton, India: Implications on the migrating arc magmatism
    C. Manikyamba, Arijit Pahari, Th. Dhanakumar Singh, Adrija Chatterjee, Sohini Ganguly
    Journal of Geodynamics, 2020
  • Meso-Neoarchean magmatism and episodic crustal growth in the Kudremukh-Agumbe granite-greenstone belt, western Dharwar Craton, India
    Arijit Pahari, Li Tang, C. Manikyamba, M. Santosh, K.S.V. Subramanyam, Sohini Ganguly
    Precambrian Research, 2019
  • Neoarchean microblock amalgamation in southern India: Evidence from the Nallamalai Suture Zone
    Shan-Shan Li, M. Santosh, Sohini Ganguly, P.V. Thanooja, K. Sajeev, Arijit Pahari, C. Manikyamba
    Precambrian Research, 2018
  • Predation on Recent Terebrid Gastropods from the Indian Subcontinent and a Spatiotemporal Reappraisal Based on a Revised Global Database
    Debattam Sarkar, Subhendu Bardhan, Subhronil Mondal, Anirban Das, Arijit Pahari, Dipankar Buragohain, Sandip Saha
    Malacologia, 2016
  • Subaerial naticid gastropod drilling predation by Natica tigrina on the intertidal molluscan community of Chandipur, Eastern Coast of India
    Arijit Pahari, Subhronil Mondal, Subhendu Bardhan, Debattam Sarkar, Sandip Saha, Dipankar Buragohain
    Palaeogeography Palaeoclimatology Palaeoecology, 2016

RECENT SCHOLAR PUBLICATIONS

  • Serpentinised Dunites of the Neoarchean Shimoga Greenstone Belt, Western Dharwar Craton, India: Insights on Ni‐PGE Mineralisation and Genesis
    T Dhanakumar Singh, C Manikyamba, G Harshitha, M Lingadevaru, ...
    Geological Journal 60 (1), 45-63 , 2025
    2025
  • Forearc and back-arc mantle characteristics of the mafic-ultramafic rocks of Simlipal complex, Singhbhum Craton, India
    C Manikyamba, M Santosh, KSV Subramanyam, GH Reddy, J Ray, A Kar, ...
    Lithos 432, 106889 , 2022
    2022
    Citations: 5
  • Arc–Back Arc Cohabitation and Associated Bimodal Volcanism: Evidence from Neoarchean Raichur Greenstone Belt, Eastern Dharwar Craton, India
    A Pahari, C Manikyamba
    Geochemical Treasures and Petrogenetic Processes, 3-29 , 2022
    2022
    Citations: 4
  • Greenstone Belt, Eastern Dharwar Craton, India
    A Pahari, C Manikyamba
    Geochemical Treasures and Petrogenetic Processes, 3 , 2022
    2022
  • Geochemistry of basalts in unravelling the mantle processes and crustal evolution: Insights from the greenstone belts of western Dharwar Craton
    C Manikyamba, A Pahari, M Santosh, KSV Subramanyam, GH Reddy
    Geosystems and Geoenvironment 1 (4), 100070 , 2022
    2022
    Citations: 14
  • Archean Biogeochemical Cognizance from Dharwar Craton, India–A Review
    C Manikyamba, CS Sindhuja, AC Khelen, A Pahari
    Journal of the Geological Society of India 98 (1), 74-78 , 2022
    2022
    Citations: 5
  • Crustal stabilization: evidence from the geochemistry and U–Pb detrital zircon geochronology of quartzites from Simlipal Complex, Singhbhum Craton, India
    CS Sindhuja, A Pahari, C Manikyamba, M Santosh, L Tang, J Ray, ...
    Geoscience Frontiers 13 (1), 101257 , 2022
    2022
    Citations: 13
  • Geochemical Features of Bellara Trap Volcanic Rocks of Chitradurga Greenstone Belt, Western Dharwar Craton, India: Insights into MORB-BABB Association from a Neoarchean Back …
    C Manikyamba, S Ganguly, A Pahari
    Journal of Earth Science 32 (6), 1528-1544 , 2021
    2021
    Citations: 10
  • Understanding the role of chalcophile-siderophile elements in the petrogenesis of metabasalts of Kudremukh greenstone belt, western Dharwar Craton, India: A Platinum group …
    A Pahari, TD Singh, C Manikyamba, KSV Subramanyam
    Journal of Earth System Science 130 (3), 168 , 2021
    2021
    Citations: 4
  • Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining crustal accretion …
    C Manikyamba, S Ganguly, M Santosh, L Tang, CS Sindhuja, A Pahari, ...
    PRECAMBRIAN RESEARCH 356 , 2021
    2021
  • Corrigendum to “Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining …
    C Manikyamba, S Ganguly, M Santosh, L Tang, CS Sindhuja, A Pahari, ...
    Precambrian Research 356, 106162 , 2021
    2021
  • Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining crustal accretion …
    C Manikyamba, S Ganguly, M Santosh, L Tang, CS Sindhuja, A Pahari, ...
    Precambrian Research 355, 106097 , 2021
    2021
    Citations: 12
  • Metallogenesis and depositional environment of the Archean-Proterozoic carbonaceous phyllites from the Dharwar Craton, India
    CS Sindhuja, C Manikyamba, A Pahari, M Santosh, L Tang
    Ore Geology Reviews 131, 103966 , 2021
    2021
    Citations: 7
  • Gold, uranium, thorium, and rare earth mineralization in the Kadiri Volcanic Province of Eastern Dharwar Craton, India: An evaluation of mineralogical, textural, and …
    C Manikyamba, NC Ghose, S Ganguly, A Pahari, CS Sindhuja
    Geological Journal 56 (1), 359-381 , 2021
    2021
    Citations: 11
  • Subduction–collision processes and crustal growth in eastern Dharwar Craton: Evidence from petrochemical studies of Hyderabad granites
    A Pahari, P Prasanth, DM Tiwari, C Manikyamba, KSV Subramanyam
    Journal of Earth System Science 129 (1), 32 , 2020
    2020
    Citations: 14
  • Mesoarchean gabbro-anorthosite complex from Singhbhum Craton, India
    C Manikyamba, A Pahari, M Santosh, J Ray, CS Sindhuja, ...
    Lithos 366, 105541 , 2020
    2020
    Citations: 38
  • Geochemistry of banded sulphidic cherts of Sandur greenstone belt, Dharwar Craton, India: Constraints on hydrothermal processes and gold mineralization
    CS Sindhuja, C Manikyamba, A Pahari, M Satyanarayanan
    Ore Geology Reviews 122, 103529 , 2020
    2020
    Citations: 15
  • Evolution of geodynamic processes in Neoarchean Kadiri greenstone belt, eastern Dharwar Craton, India: implications on the migrating arc magmatism
    C Manikyamba, A Pahari, T Dhanakumar, A Chatterjee, S Ganguly
    Journal of Geodynamics, 101717 , 2020
    2020
    Citations: 15
  • Zircon Thermometry and Trace Element Signatures: Implications on Crustal Growth of the Western Dharwar Craton, India
    A Pahari, M Maningri
    Twenty-ninth Annual Goldschmidt Conference, 2553 , 2019
    2019
  • Meso-Neoarchean magmatism and episodic crustal growth in the Kudremukh-Agumbe granite-greenstone belt, western Dharwar Craton, India
    A Pahari, L Tang, C Manikyamba, M Santosh, KSV Subramanyam, ...
    Precambrian Research 323, 16-54 , 2019
    2019
    Citations: 32

MOST CITED SCHOLAR PUBLICATIONS

  • Neoarchean microblock amalgamation in southern India: Evidence from the Nallamalai Suture Zone
    SS Li, M Santosh, S Ganguly, PV Thanooja, K Sajeev, A Pahari, ...
    Precambrian Research 314, 1-27 , 2018
    2018
    Citations: 45
  • Subaerial naticid gastropod drilling predation by Natica tigrina on the intertidal molluscan community of Chandipur, Eastern Coast of India
    A Pahari, S Mondal, S Bardhan, D Sarkar, S Saha, D Buragohain
    Palaeogeography, Palaeoclimatology, Palaeoecology 451, 110-123 , 2016
    2016
    Citations: 43
  • Mesoarchean gabbro-anorthosite complex from Singhbhum Craton, India
    C Manikyamba, A Pahari, M Santosh, J Ray, CS Sindhuja, ...
    Lithos 366, 105541 , 2020
    2020
    Citations: 38
  • Meso-Neoarchean magmatism and episodic crustal growth in the Kudremukh-Agumbe granite-greenstone belt, western Dharwar Craton, India
    A Pahari, L Tang, C Manikyamba, M Santosh, KSV Subramanyam, ...
    Precambrian Research 323, 16-54 , 2019
    2019
    Citations: 32
  • Geochemistry of banded sulphidic cherts of Sandur greenstone belt, Dharwar Craton, India: Constraints on hydrothermal processes and gold mineralization
    CS Sindhuja, C Manikyamba, A Pahari, M Satyanarayanan
    Ore Geology Reviews 122, 103529 , 2020
    2020
    Citations: 15
  • Evolution of geodynamic processes in Neoarchean Kadiri greenstone belt, eastern Dharwar Craton, India: implications on the migrating arc magmatism
    C Manikyamba, A Pahari, T Dhanakumar, A Chatterjee, S Ganguly
    Journal of Geodynamics, 101717 , 2020
    2020
    Citations: 15
  • Geochemistry of basalts in unravelling the mantle processes and crustal evolution: Insights from the greenstone belts of western Dharwar Craton
    C Manikyamba, A Pahari, M Santosh, KSV Subramanyam, GH Reddy
    Geosystems and Geoenvironment 1 (4), 100070 , 2022
    2022
    Citations: 14
  • Subduction–collision processes and crustal growth in eastern Dharwar Craton: Evidence from petrochemical studies of Hyderabad granites
    A Pahari, P Prasanth, DM Tiwari, C Manikyamba, KSV Subramanyam
    Journal of Earth System Science 129 (1), 32 , 2020
    2020
    Citations: 14
  • Predation on Recent terebrid gastropods from the Indian subcontinent and a spatiotemporal reappraisal based on a revised global database
    D Sarkar, S Bardhan, S Mondal, A Das, A Pahari, D Buragohain, S Saha
    Malacologia 59 (2), 271-302 , 2016
    2016
    Citations: 14
  • Crustal stabilization: evidence from the geochemistry and U–Pb detrital zircon geochronology of quartzites from Simlipal Complex, Singhbhum Craton, India
    CS Sindhuja, A Pahari, C Manikyamba, M Santosh, L Tang, J Ray, ...
    Geoscience Frontiers 13 (1), 101257 , 2022
    2022
    Citations: 13
  • Tectonic juxtaposition of plume and subduction derived magmatic sequences in the Bababudan greenstone terrane, western Dharwar Craton, India: Constraining crustal accretion …
    C Manikyamba, S Ganguly, M Santosh, L Tang, CS Sindhuja, A Pahari, ...
    Precambrian Research 355, 106097 , 2021
    2021
    Citations: 12
  • Gold, uranium, thorium, and rare earth mineralization in the Kadiri Volcanic Province of Eastern Dharwar Craton, India: An evaluation of mineralogical, textural, and …
    C Manikyamba, NC Ghose, S Ganguly, A Pahari, CS Sindhuja
    Geological Journal 56 (1), 359-381 , 2021
    2021
    Citations: 11
  • Geochemical Features of Bellara Trap Volcanic Rocks of Chitradurga Greenstone Belt, Western Dharwar Craton, India: Insights into MORB-BABB Association from a Neoarchean Back …
    C Manikyamba, S Ganguly, A Pahari
    Journal of Earth Science 32 (6), 1528-1544 , 2021
    2021
    Citations: 10
  • Metallogenesis and depositional environment of the Archean-Proterozoic carbonaceous phyllites from the Dharwar Craton, India
    CS Sindhuja, C Manikyamba, A Pahari, M Santosh, L Tang
    Ore Geology Reviews 131, 103966 , 2021
    2021
    Citations: 7
  • Forearc and back-arc mantle characteristics of the mafic-ultramafic rocks of Simlipal complex, Singhbhum Craton, India
    C Manikyamba, M Santosh, KSV Subramanyam, GH Reddy, J Ray, A Kar, ...
    Lithos 432, 106889 , 2022
    2022
    Citations: 5
  • Archean Biogeochemical Cognizance from Dharwar Craton, India–A Review
    C Manikyamba, CS Sindhuja, AC Khelen, A Pahari
    Journal of the Geological Society of India 98 (1), 74-78 , 2022
    2022
    Citations: 5
  • Arc–Back Arc Cohabitation and Associated Bimodal Volcanism: Evidence from Neoarchean Raichur Greenstone Belt, Eastern Dharwar Craton, India
    A Pahari, C Manikyamba
    Geochemical Treasures and Petrogenetic Processes, 3-29 , 2022
    2022
    Citations: 4
  • Understanding the role of chalcophile-siderophile elements in the petrogenesis of metabasalts of Kudremukh greenstone belt, western Dharwar Craton, India: A Platinum group …
    A Pahari, TD Singh, C Manikyamba, KSV Subramanyam
    Journal of Earth System Science 130 (3), 168 , 2021
    2021
    Citations: 4
  • Serpentinised Dunites of the Neoarchean Shimoga Greenstone Belt, Western Dharwar Craton, India: Insights on Ni‐PGE Mineralisation and Genesis
    T Dhanakumar Singh, C Manikyamba, G Harshitha, M Lingadevaru, ...
    Geological Journal 60 (1), 45-63 , 2025
    2025
  • Greenstone Belt, Eastern Dharwar Craton, India
    A Pahari, C Manikyamba
    Geochemical Treasures and Petrogenetic Processes, 3 , 2022
    2022