Bapi Goswami

@caluniv.ac.in

Associate Professor, Deoartment of Geology, Faculty of Science
University of Calcutta

Bapi Goswami


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https://researchid.co/bapigoswami69

RESEARCH, TEACHING, or OTHER INTERESTS

Geology, Geochemistry and Petrology, Environmental Science
25

Scopus Publications

360

Scholar Citations

12

Scholar h-index

14

Scholar i10-index

Scopus Publications

  • Corrigendum to “A novel fossil-species of Meliolinites Selkirk (fossil Meliolaceae) and its life cycle stages associated with an angiosperm fossil leaf from the Siwalik (Mio-Pliocene) of Bhutan sub-Himalaya”(Fungal Biology, (2022), 126, 9, (576-586), (S1878614622000770), 10.1016/j.funbio.2022.07.003)
    Meghma Bera, Mahasin Ali Khan, Taposhi Hazra, Krishnendu Acharya, Bapi Goswami, Subir Bera
    Fungal Biology, 2026
  • Geochemistry and petrogenesis of basement grey granitoid gneisses from the Chhotanagpur Gneissic Complex, eastern India: Implications for the Mesoproterozoic continental arc magmatism
    Sukhendu Ray, Bapi Goswami, Yoann Gréau, Chittaranjan Bhattacharyya
    Acta Geochimica, 2026
  • Antiquity of tritrophic interaction in black mildew: Evidence from the Neogene Siwalik forest of Arunachal Sub-Himalaya
    Meghma Bera, Shreyasi Basak, Roland Kirschner, Mahasin Ali Khan, Dipak Kumar Paruya, Robert A. Spicer, Krishnendu Acharya, Bapi Goswami, Subir Bera
    Mycologia, 2026
    The present work is the first fossil evidence of fungi associated with black mildew fungi, Meliolales. Here we present the occurrence of three different fungicolous fungi colonizing members of Meliolinites (fossil taxonomic equivalent of extant Meliola) on three different compressed angiosperm host leaves from middle-upper Siwalik strata (Pliocene to Early Pleistocene) of Arunachal Pradesh, eastern Himalaya. We suggest that the fossil fungicolous fungi were biological stressors of the black mildew in a potential tritrophic interaction in the tropical palaeoenvironment of middle-upper Siwalik forest of Arunachal Sub-Himalaya.
  • Tonian shoshonitic to ultrapotassic granitoids from Chhotanagpur Gneissic Complex, Eastern Indian Shield: Age, origin and tectonic implications
    Ankita Basak, Bapi Goswami, Yoann Gréau, Susmita Das, Chittaranjan Bhattacharyya
    Geosystems and Geoenvironment, 2025
    • Ultrapotassic, high Ba-Sr granitoids in the Chhotanagpur Gneissic Complex. • Granitoid magma was generated by anatexis of shoshonitic hornblende granulites. • Preservation of magmatic epidote indicate rapid ascent of granitoid magma. • Mafic magmas severed as an essential driving force for anataxis. • New geochemical diagrams to discriminate mantle vs. crustal sources of granitoids. This work reports petrogenesis of an ultrapotassic granitoid pluton emplaced in the Tonian (949.4 ± 2.3 Ma; new LA-ICPMS zircon U–Pb dating) along a regional shear zone during the post-collisional stage of the Grenvillian Satpura orogeny in Eastern India. The hypidiomorphic granitoids comprise dominantly perthite, microcline (BaO up to 5.85 wt.%), quartz, albite and subordinate amphibole ± diopside ± epidote, allanite, titanite, magnetite ± ilmenite ± biotite ± calcite. Preservation of magmatic epidotes and resorbed boundaries indicates rapid ascent of the granitoid magma. Mylonitic deformation overprinted the southern part of the E-W trending pluton. Magmatic epidote with resorbed boundaries suggests rapid magma ascent. The metaluminous granitoids display affinities with shoshonitic rocks, i.e., enrichment of K 2 O (5.79–11.41 wt.%), large ion lithophile elements (Ba 461.5–7004.8 ppm; Sr 151.3–3548.3 ppm), light rare earth elements (LREE 111.2–1317.7 ppm) and high K 2 O/Na 2 O (1.77–11.35) and La CN /Yb CN (11.7–82.48) ratios with both negative and positive Eu-anomalies (Eu/Eu* = 0.58–1.43; average 0.89). Trace element characteristics of zircons demonstrate their magmatic origin. Pseudosection modeling displays high temperature (∼800°C), high f O 2 (ΔNNO +0.8 to +2.6), and CO 2 activity (0.9) of the magma that intruded at shallow crustal depth (∼300 MPa). Biotite remains unstable at this physicochemical condition of the shoshonitic magma. Metaluminous nature, high (La/Yb) CN (11.7–82.48) and Sr/Y (6.46–277.21) ratios, and Nb/U (avg. 7.4), Ce/Pb (avg. 6.8), Nb/Ta (avg. 11.9), Zr/Hf (avg. 31.61), and low Rb/Sr (0.09–1.39) ratios of these rocks indicate the derivation of the magma from partial melting of the mafic lower crust. Batch melting modeling shows the granitoid magma originated from 5 to 30 % batch melting of K–Ba–Sr-rich shoshonitic mafic (hornblende granulite) source. The study proposes new (Ba + Sr)–Ti–P and Ba–Sr–Ti triangular diagrams for distinguishing mantle vs. crustal sources of post-collisional granitoids.
  • Geochemistry and petrogenesis of Mesoproterozoic mafic granulite and amphibolite dykes from Saltora, Bankura district, Chhotanagpur Gneissic Complex, eastern India: Implications for their emplacement in within-plate setting
    Poulami Roy, , Bapi Goswami, Ankita Basak, Anwesa Sen, Chittaranjan Bhattacharyya
    China Geology, 2025
    Distinguishing high-grade mafic-ultramafic rocks originally crystallized from within-plate basaltic magmatism is challenging and crucial because the chemical composition of the igneous rocks has been modified during high-grade metamorphism, causing misidentification of the characters of the parental magma. Proterozoic metamorphosed mafic dykes occur throughout the Chhotanagpur Gneissic Complex (CGC) of eastern Indian shield. The E-W trending mafic dykes from the Saltora area in the southeastern CGC underwent metamorphism in two episodes: M<sub>1</sub> ( 650 MPa; 770°C) and M<sub>2</sub> (300 MPa; 744°C). The metamafics are enriched in LILE, depleted in HFSE, and display strong fractionation of LREE, nearly flat HREE patterns in a chondrite-normalized REE diagram, and show tholeiitic differentiation trend. Their geochemical affinity is towards rift-related, continental within-plate basalts. About 7%–10% melting of the carbonated spinel-peridotite sub-continental lithospheric mantle (SCLM) produced the parental mafic magma. The pre-existing SCLM was metasomatized by slab-derived fluid during the previous subduction. The upwelling of the asthenosphere in a post-collisional tectonic setting caused E-W trending fractures, lithospheric thinning, and gravitational collapse. These dykes were emplaced during crustal extension around 1070 Ma. The remarkable geochemical similarity between the mafic dykes of Saltora and Dhanbad, the ca. 1096 Ma Mahoba (Bundelkhand craton), and the ca. 1070 Ma Alcurra mafic dykes in Australia supports a genetic link.
  • Petrogenesis of post-collisional mesozonal enderbite in the Proterozoic Chhotanagpur Gneissic Complex, Eastern India: Implications of slab-break-off
    Poulami Roy, Bapi Goswami, Ankita Basak, Chittaranjan Bhattacharyya
    Solid Earth Sciences, 2024
    Collisional orogeny produces large volumes of tonalitic melts at two stages: first, during the oceanic subduction below the continent (continental arc), and again, during the post-collisional stage. In a polydeformed and polymetamorphosed terrain, it would be challenging to distinguish between arc tonalites and post-collisional tonalites (and their metamorphosed equivalents, enderbites). The Chhotanagpur Gneissic Complex (CGC) belongs to the EW to ENE-WSW tending, 1500 km long Grenvillian collisional belt amalgamating the North and South Indian cratonic blocks. We discuss the field disposition, petrography, mineral chemistry, geochemistry, the physical condition of crystallization and metamorphism, and the petrogenetic model of enderbites from the CGC. Enderbites sporadically occur as cm-to-dm-thick leucosomal bands in migmatitic gneisses (migmatitic enderbites) and as small stock-sized plutons (massive enderbites) intruding migmatitic gneisses. Both of these types intruded before the end of the regional deformation. Both the massive and migmatitic enderbites predominantly contain plagioclase, quartz, biotite (with a higher abundance in the migmatitic type), minor orthopyroxene, clinopyroxene, hornblende, K-feldspar, and accessories such as opaque minerals, apatite, and zircon. Garnets rarely occur in migmatitic enderbites. Thermodynamic modeling suggests a low liquidus temperature (∼750 °C), intermediate pressure of emplacement (∼5.5 kb), moderate oxygen fugacity (ΔQFM = +1 to +2), and low water (∼4.0 wt%) of the parental tonalite magma. The two enderbite types have been derived from two distinct crustal (amphibolites) sources by water-fluxed partial melting at <10 kb pressure, shallower than the garnet stability field. About 20–40 % of batch-melting of shoshonitic basaltic sources yielded migmatitic enderbites, while about 40–70 % of batch-melting of within-plate basaltic sources produced massive enderbites. Discrimination diagrams display a post-collision tectonic setting of these enderbites. The migmatitic enderbites and magma of enderbite plutons formed during regional anatexis due to thermal relaxation in the lower crust after attaining peak pressure during the decompressive phase of regional granulite facies metamorphism (1000–950 Ma) related to slab breakoff at the post-collisional stage of the orogeny. Mantle-derived magmas formed by adiabatic decompression in the upper mantle supplied the heat. • Enderbites occur both as leucosomes in migmatites and in discrete plutonic massifs. • Petrography, mineral chemistry, geochemistry, and metamorphism of post-collisional enderbites • Water-fluxed melting of geochemically distinct amphibolite sources for parental magmas of enderbites • Geodynamic implications of amphibolite melting during the Grenvillian collisional orogeny.
  • Petrogenesis of Late Stenian Syn-Orogenic A-Type Granites in the Chhotanagpur Gneissic Complex and Eastern Indian Shield
    Bapi Goswami, Ankita Basak, Yoann Gréau, Chittaranjan Bhattacharyya
    Minerals, 2024
    We report the petrogenesis of arfvedsonite granites from the Dimra Pahar pluton in the Chhotanagpur Gneissic Complex based on petrology, whole-rock chemistry, mineral chemistry, and La-ICP-MS zircon U-Pb ages and Hf-Lu isotopic analyses. These granites are dominantly peralkaline, occasionally peraluminous, and demonstrate features of A1-type granites. The magma was emplaced at a shallow depth and had a high liquidus temperature, fO2 (&gt;NNO), and water saturation. The zircons exhibit three distinct U-Pb isotopic ages. The oldest (1324 ± 6 Ma), large-sized inherited zircons (εHf(t) = +1.65 to +7.64), show complex zoning and signs of partial resorption. The euhedral, prismatic-bipyramidal zircons displaying oscillatory zoning (εHf(t) = −3.43 to +1.43) reveal a crystallization age of 1046 ± 7 Ma. Their thin periphery (εHf(t) = −3.23 to +0.27) grew during retrograde metamorphism (995 ± 6 Ma). The whole-rock geochemistry and the Hf-isotope values imply that the parental magma of these granites resulted from the anatexis of metasomatized lithospheric mantle sources. These granites intruded in a syn-orogenic (syn-collisional exhumation) stage of the orogeny.
  • Discovery of Early Tonian Calc-alkaline and Shoshonitic Metamafic Rocks from the North Purulia Shear Zone, Chhotanagpur Gneissic Complex, Eastern India: Implications of Proterozoic Sub-continental Lithospheric Mantle
    Bapi GOSWAMI, Susmita DAS, Ankita BASAK, Chitta BHATTACHARYYA
    Acta Geologica Sinica English Edition, 2023
    Reports of shoshonitic rocks in Precambrian terrains are relatively rare. Pl‐Grt amphibolites and Hbl‐Bt mafic granulites occurring in the migmatitic gneisses of the Chhotanagpur Gneissic Complex (CGC) show calc‐alkaline and shoshonitic characteristics. Relict porphyritic, sub‐ophitic and poikilitic textures are noted in these rocks. Their parent magma was emplaced during the waning phase of the regional metamorphism. Geochemically, these metamafics are similar to the Group III potassic and ultrapotassic rocks of Foley et al. (1987). The magma was derived from the metasomatized subcontinental lithospheric mantle (SCLM). Subduction‐related sediment melts metasomatized the SCLM. Compositionally, the SCLM is a metasomatized phlogopite‐amphibole‐spinel‐bearing harzburgite. 1%–5% batch melting of the SCLM could produce the parental magma of the mafic granulites. Pressures and temperatures of metamorphic equilibration were carried out by pseudosection modeling. Peak metamorphic assemblage (M1: Grt‐Cpx‐Pl‐Qz) in garnetiferous amphibolite equilibrated at 740°C and 8.7 kbar. The Cpx‐Pl corona appeared around the garnet during decompression (M2: 655°C, 6 kbar). The Hbl‐Pl symplectites around garnet formed during isobaric cooling (M3: 580°C and 5.9 kbar). The emplacement of shoshonitic magma and subsequent decompression happened at the slab break‐off stage of continental collision (∼990 Ma).
  • Occurrence of foliicolous fungus Zygosporium Mont. (Zygosporiaceae) from the Mio-Pliocene of eastern Himalaya
    Meghma Bera, Shreyasi Basak, Mahasin Ali Khan, Dipak Kumar Paruya, Bapi Goswami, Krishnendu Acharya, Subir Bera
    Review of Palaeobotany and Palynology, 2023
  • A novel fossil-species of Meliolinites Selkirk (fossil Meliolaceae) and its life cycle stages associated with an angiosperm fossil leaf from the Siwalik (Mio-Pliocene) of Bhutan sub-Himalaya
    Meghma Bera, Mahasin Ali Khan, Taposhi Hazra, Krishnendu Acharya, Bapi Goswami, Subir Bera
    Fungal Biology, 2022
    Here, we report the in-situ occurrence of a new fossil-species of Meliolinites (fossil Meliolaceae), Meliolinites bhutanensis sp. nov. on the cuticle fragments of a compressed angiosperm dicot leaf recovered from the middle Siwalik (Formation II: latest Miocene to Pliocene) of Bhutan, eastern Himalaya. This unique foliicolous new fossil fungal species features well-preserved mycelia consisting of superficial, brown to dark brown, septate, thick-walled, branching hyphae with bi-cellular appressoria, unicellular phialides, and a characteristic long, slightly curved hyphal seta. The web-like, brown to dark brown fungal colonies also include globose to sub-globose, dark brown ascomata, and oblong to broadly cylindrical, 5-celled, 4-septate, brown to dark brown, mature ascospores. As almost all features of different stages in the life cycle (ascospores, mature germinating ascospores, superficial lateral hyphae, hyphal seta, hyphopodia, mycelial colony, and ascomata) of this new fossil-species are found, we have proposed the first time a possible life cycle of fossil-species of Meliolaceae. The in-situ evidence of M. bhutanensis on the host leaf cuticle indicates the possible existence of a host-ectoparasite relationship in Bhutan sub-Himalaya's ancient warm and humid tropical evergreen forest during the deposition. So, M. bhutanensis might have thrived generally under warm and humid climate conditions for its growth and development in the Mio-Pliocene time, which is in conformity with our recently published quantitative climatic data by CLAMP (Climate Leaf Analysis Multivariate Program) analysis.
  • Petrogenesis of the post-collisional porphyritic granitoids from Jhalida, Chhotanagpur Gneissic Complex, eastern India
    Poulami Roy, Bapi Goswami, Sukanya Dutta, Chittaranjan Bhattacharyya
    Geological Magazine, 2021
  • Physico-chemical conditions of crystallization and composition of source magma of the Grenvillian post-collisional mafic–ultramafic rocks in the Chhotanagpur Gneissic Complex, Eastern India
    Susmita Das, Bapi Goswami, Chittaranjan Bhattacharyya
    Journal of Earth System Science, 2020
  • A Grenvillian magmatic almandine garnet-bearing ferroan granite intrusion in the Chhotanagpur Gneissic complex, Eastern India: Petrology, petrochemistry, petrogenesis and geodynamic implications
    Susmita Das, Bapi Goswami, Ankita Basak, Chitta Bhattacharyya
    Lithos, 2020
  • The physico-chemical conditions of crystallization of the Grenvillian arfvedsonite granite of Dimra Pahar, Hazaribagh, India: constraints on possible source regions
    Ankita Basak, Bapi Goswami
    Mineralogy and Petrology, 2020
  • Magmatic epidote in the Grenvillian granitoids of North Purulia Shear Zone, Chhotanagpur Gneissic Complex, India and its significance
    Ankita Basak, Bapi Goswami, Ananya Singha, Somshubhra Das, Chitta Bhattacharyya
    Current Science, 2019
  • Physico-chemical conditions of four calc-alkaline granitoid plutons of Chhotanagpur Gneissic Complex, eastern India: Tectonic implications
    B Goswami, P Roy, A Basak, S Das, C Bhattacharyya
    Journal of Earth System Science, 2018
  • Petrogenesis of shoshonitic granitoids, Eastern India: Implications for the late Grenvillian post-collisional magmatism
    B. Goswami, C. Bhattacharyya
    Geoscience Frontiers, 2014
  • Metamorphism of Proterozoic agpaitic nepheline syenite gneiss from North Singhbhum Mobile Belt, eastern India
    Bapi Goswami, Swades Kumar Basu
    Mineralogy and Petrology, 2013
  • Developing GIS-based techniques for application of knowledge and data-driven methods of landslide susceptibility mapping
    Indian Journal of Geosciences, 2013
  • Understanding the transportational and depositional setting of Panchet Formation, Purulia and Bankura districts of West Bengal, India - Evidence from grain size analysis
    Bapi Goswami, Dipsikha Ghosh
    Frontiers of Earth Science, 2011
  • Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley), eastern India
    ABHIK KUNDU, BAPI GOSWAMI, PATRICK G ERIKSSON, ABHIJIT CHAKRABORTY
    Journal of Earth System Science, 2011
  • Discussion: Petrology of mafic-ultramafic rocks along north Purulia Shear Zone, West Bengal
    B. Goswami, C. Bhattacharyya, Aditi Mandal, Arijit Ray
    Journal of the Geological Society of India, 2009
  • Discussion on the paper "On charnockites" published in Gondwana Research, volume 13, 30-44 (2008) by B.Ronald Frost & Carol D. Frost
    C. Bhattacharyya, B. Goswami
    Gondwana Research, 2009
  • A note on seismic evidences during the sedimentation of panchet formation, Damodar basin, Eastern India: Banspetali Nullah revisited
    Journal of the Geological Society of India, 2008
  • Metamorphism of nepheline syenite gneisses from Chhotanagpur granite gneiss complex, Northeastern Puruliya district, Eastern India
    Journal of the Geological Society of India, 2008

RECENT SCHOLAR PUBLICATIONS

  • Geochemistry and petrogenesis of basement grey granitoid gneisses from the Chhotanagpur Gneissic Complex, eastern India: Implications for the Mesoproterozoic continental arc …
    S Ray, B Goswami, Y Gréau, C Bhattacharyya
    Acta Geochimica, 1-29 , 2026
    2026
  • Corrigendum to" A novel fossil-species of Meliolinites Selkirk (fossil Meliolaceae) and its life cycle stages associated with an angiosperm fossil leaf from the Siwalik (Mio …
    M Bera, MA Khan, T Hazra, K Acharya, B Goswami, S Bera
    Fungal biology 130 (2), 101735 , 2026
    2026
  • Petrology, geochemistry and petrogenesis of Stenian alkaline intrusions from the Chhotanagpur Gneissic Complex, Eastern Indian shield
    B Goswami, A Basak, Y Greau
    Goldschmidt 2025 Conference , 2025
    2025
  • Tonian shoshonitic to ultrapotassic granitoids from Chhotanagpur Gneissic Complex, Eastern Indian Shield: Age, origin and tectonic implications
    A Basak, B Goswami, Y Gréau, S Das, C Bhattacharyya
    Geosystems and Geoenvironment 4 (2), 100373 , 2025
    2025
    Citations: 3
  • Geochemistry and petrogenesis of Mesoproterozoic mafic granulite and amphibolite dykes from Saltora, Bankura district, Chhotanagpur Gneissic Complex, eastern India …
    P Roy, B Goswami, A Basak, A Sen, C Bhattacharyya
    China Geology 8 (1), 159-186 , 2025
    2025
    Citations: 2
  • Tonian shoshonitic to ultrapotassic granitoids from Chhotanagpur Gneissic Complex, Eastern Indian Shield
    A Basak, B Goswami, Y Gréau, S Das, C Bhattacharyya
    2025
  • GIS based delineation of groundwater prospective zones using AHP techniques in Jaldhaka watershed, Cooch Behar district, West Bengal
    T Basu, A Chatterjee, B Goswami
    J Environ Pharm Sustain Sci 2 (01), 1-20 , 2025
    2025
    Citations: 1
  • China Geology
    P Roy, B Goswami, A Basak, A Sen, C Bhattacharyya
    2025
  • Petrogenesis of post-collisional mesozonal enderbite in the Proterozoic Chhotanagpur Gneissic Complex, Eastern India: Implications of slab-break-off
    P Roy, B Goswami, A Basak, C Bhattacharyya
    Solid Earth Sciences 9 (4), 100217 , 2024
    2024
    Citations: 1
  • Petrogenesis of late stenian syn-orogenic A-type granites in the Chhotanagpur Gneissic Complex and Eastern Indian Shield
    B Goswami, A Basak, Y Gréau, C Bhattacharyya
    Minerals 14 (11), 1153 , 2024
    2024
    Citations: 3
  • Discovery of Early Tonian Calc‐alkaline and Shoshonitic Metamafic Rocks from the North Purulia Shear Zone, Chhotanagpur Gneissic Complex, Eastern India: Implications of …
    B Goswami, S Das, A Basak, C Bhattacharyya
    Acta Geologica Sinica‐English Edition 97 (1), 68-89 , 2023
    2023
    Citations: 5
  • Occurrence of foliicolous fungus Zygosporium Mont.(Zygosporiaceae) from the Mio-Pliocene of eastern Himalaya
    M Bera, S Basak, MA Khan, DK Paruya, B Goswami, K Acharya, S Bera
    Review of Palaeobotany and Palynology 309, 104803 , 2023
    2023
    Citations: 6
  • A novel fossil-species of Meliolinites Selkirk (fossil Meliolaceae) and its life cycle stages associated with an angiosperm fossil leaf from the Siwalik (Mio-Pliocene) of …
    M Bera, MA Khan, T Hazra, K Acharya, B Goswami, S Bera
    Fungal Biology 126 (9), 576-586 , 2022
    2022
    Citations: 12
  • Petrology, geochemistry, and petrogenesis of calcic-ferroan-metaluminous garnetiferous magmatic charnockites from eastern Chhotanagpur Gneissic Complex, Eastern Indian Craton
    B Goswami, S Das, A Basak, C Bhattacharyya, C Goswami
    EGU General Assembly Conference Abstracts, EGU22-6214 , 2022
    2022
  • Studies on Mineral Resources of Cerium
    B Goswami, CK Goswami
    International Journal of Solid State Materials 7 (1), 14-18 , 2021
    2021
  • Petrogenesis of the post-collisional porphyritic granitoids from Jhalida, Chhotanagpur Gneissic Complex, eastern India
    P Roy, B Goswami, S Dutta, C Bhattacharyya
    Geological Magazine 158 (4), 598-634 , 2021
    2021
    Citations: 8
  • A Grenvillian magmatic almandine garnet-bearing ferroan granite intrusion in the Chhotanagpur Gneissic complex, Eastern India: Petrology, petrochemistry, petrogenesis and …
    S Das, B Goswami, A Basak, C Bhattacharyya
    Lithos 376, 105749 , 2020
    2020
    Citations: 20
  • Physico-chemical conditions of crystallization and composition of source magma of the Grenvillian post-collisional mafic–ultramafic rocks in the Chhotanagpur Gneissic Complex …
    S Das, B Goswami, C Bhattacharyya
    Journal of Earth System Science 129 (1), 89 , 2020
    2020
    Citations: 10
  • The physico-chemical conditions of crystallization of the Grenvillian arfvedsonite granite of Dimra Pahar, Hazaribagh, India: constraints on possible source regions
    B Ankita, G Bapi
    Mineralogy and Petrology 114 (4), 329-356 , 2020
    2020
    Citations: 15
  • Magmatic epidote in the grenvillian granitoids of North Purulia Shear Zone, Chhotanagpur Gneissic Complex, India and its significance
    A Basak, B Goswami, A Singha, S Das, C Bhattacharyya
    Current Science 117 (2), 298-303 , 2019
    2019
    Citations: 9

MOST CITED SCHOLAR PUBLICATIONS

  • Petrogenesis of shoshonitic granitoids, eastern India: implications for the late Grenvillian post-collisional magmatism
    B Goswami, C Bhattacharyya
    Geoscience Frontiers 5 (6), 821-843 , 2014
    2014
    Citations: 70
  • Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley …
    A Kundu, B Goswami, PG Eriksson, A Chakraborty
    Journal of Earth System Science 120 (1), 167-181 , 2011
    2011
    Citations: 41
  • Tectonothermal evolution of Chhotanagpur granite gneiss complex from northeastern part of Puruliya district, West Bengal, eastern India
    B Goswami, C Bhattacharyya
    Ind. J. Geol 80 (1-4), 41-54 , 2008
    2008
    Citations: 34
  • A Grenvillian magmatic almandine garnet-bearing ferroan granite intrusion in the Chhotanagpur Gneissic complex, Eastern India: Petrology, petrochemistry, petrogenesis and …
    S Das, B Goswami, A Basak, C Bhattacharyya
    Lithos 376, 105749 , 2020
    2020
    Citations: 20
  • A Note on Scismic Evidences during the Sedimentation of Panchet Formation, Damodar Basin, Eastern India: Banspetali Nullah Revisited
    A Kundu, B Goswami
    Journal of the Geological Society of India 72 (3), 400-404 , 2008
    2008
    Citations: 17
  • Physico-chemical conditions of four calc-alkaline granitoid plutons of Chhotanagpur Gneissic Complex, eastern India: Tectonic implications
    B Goswami, P Roy, A Basak, S Das, C Bhattacharyya
    Journal of Earth System Science 127 (8), 120 , 2018
    2018
    Citations: 16
  • Metamorphism of Proterozoic agpaitic nepheline syenite gneiss from North Singhbhum Mobile Belt, eastern India
    B Goswami, SK Basu
    Mineralogy and Petrology 107 (4), 517-538 , 2013
    2013
    Citations: 16
  • Magur (Clarias batrachus) seed production using low cost hatcheries: A participatory approach in Dakshin Dinajpur District of West Bengal, India
    B Goswami
    Aquaculture Asia 12 (3), 14 , 2007
    2007
    Citations: 16
  • The physico-chemical conditions of crystallization of the Grenvillian arfvedsonite granite of Dimra Pahar, Hazaribagh, India: constraints on possible source regions
    B Ankita, G Bapi
    Mineralogy and Petrology 114 (4), 329-356 , 2020
    2020
    Citations: 15
  • Understanding the transportational and depositional setting of Panchet Formation, Purulia and Bankura districts of West Bengal, India—Evidence from grain size analysis
    B Goswami, D Ghosh
    Frontiers of Earth Science 5 (2), 138-149 , 2011
    2011
    Citations: 15
  • Developing GIS-based techniques for application of knowledge and data-driven methods of landslide susceptibility mapping
    S Ghosh, R Das, B Goswami
    Indian Journal of Geosciences 67 (3-4), 249-272 , 2013
    2013
    Citations: 14
  • Metamorphism of nepheline syenite gneisses from Chhotanagpur Granite Gneiss Complex, northeastern Puruliya district, eastern India
    B Goswami, C Bhattacharyya
    Journal of the Geological Society of India 71 (2), 209-213 , 2008
    2008
    Citations: 14
  • A novel fossil-species of Meliolinites Selkirk (fossil Meliolaceae) and its life cycle stages associated with an angiosperm fossil leaf from the Siwalik (Mio-Pliocene) of …
    M Bera, MA Khan, T Hazra, K Acharya, B Goswami, S Bera
    Fungal Biology 126 (9), 576-586 , 2022
    2022
    Citations: 12
  • Physico-chemical conditions of crystallization and composition of source magma of the Grenvillian post-collisional mafic–ultramafic rocks in the Chhotanagpur Gneissic Complex …
    S Das, B Goswami, C Bhattacharyya
    Journal of Earth System Science 129 (1), 89 , 2020
    2020
    Citations: 10
  • Magmatic epidote in the grenvillian granitoids of North Purulia Shear Zone, Chhotanagpur Gneissic Complex, India and its significance
    A Basak, B Goswami, A Singha, S Das, C Bhattacharyya
    Current Science 117 (2), 298-303 , 2019
    2019
    Citations: 9
  • Petrogenesis of the post-collisional porphyritic granitoids from Jhalida, Chhotanagpur Gneissic Complex, eastern India
    P Roy, B Goswami, S Dutta, C Bhattacharyya
    Geological Magazine 158 (4), 598-634 , 2021
    2021
    Citations: 8
  • Mantle metasomatism of ultramafic intrusives in Chhotanagpur Granite Gneiss Complex, Puruliya District, West Bengal, eastern India: Evidence from trace element and REE geochemistry
    A Mandal, B Goswami, S Mukherjee, S Das, I Bhattacharyya, ...
    Igneous Petrology: 21st Century Perspective, 122-142 , 2007
    2007
    Citations: 7
  • Occurrence of foliicolous fungus Zygosporium Mont.(Zygosporiaceae) from the Mio-Pliocene of eastern Himalaya
    M Bera, S Basak, MA Khan, DK Paruya, B Goswami, K Acharya, S Bera
    Review of Palaeobotany and Palynology 309, 104803 , 2023
    2023
    Citations: 6
  • Discovery of Early Tonian Calc‐alkaline and Shoshonitic Metamafic Rocks from the North Purulia Shear Zone, Chhotanagpur Gneissic Complex, Eastern India: Implications of …
    B Goswami, S Das, A Basak, C Bhattacharyya
    Acta Geologica Sinica‐English Edition 97 (1), 68-89 , 2023
    2023
    Citations: 5
  • Discussion on the paper “On charnockites” published in Gondwana Research, volume 13, 30–44 (2008) by B. Ronald Frost & Carol D. Frost
    C Bhattacharyya, B Goswami
    Gondwana Research 15 (2), 216-217 , 2009
    2009
    Citations: 4