Permian Carbonaceous Shales From Raniganj Sub-Basin—A Potential Source of Hydrocarbons? Inferences Drawn From Kerogen Characteristics and Kinetics Monalisa Mallick, Barnita Banerjee, Nihar Ranjan Kar, Runcie Paul Mathews, Vikram P. Singh, Manish Tiwari, E. V. S. S. K. Babu, Tanveer Hassan, Satendra Kumar Gupta Geological Journal, 2026 The present study reports a geochemical evaluation of Permian aged Raniganj, Barren Measure and Barakar shales from R1 and R4 boreholes from the NE part of the Raniganj sub‐basin. We have investigated organic matter characteristics, stable isotopic composition, hydrocarbon potential and kerogen kinetics to decipher shale gas potential as well as artificial hydrocarbon generation prospect. The shales contain high total organic carbon (TOC) content ~2.5–26.5 wt%, mainly Type III kerogen with minor Type II/III kerogen. The provenance of organic matters has been determined using δ13Corg and δ15Nbulk composition and Total Nitrogen content to be predominantly terrestrial deposited primarily in an oxic to suboxic environment. Kinetic parameters for kerogen degradation reactions namely, activation energies (Ea) distribution, frequency factors are in the range of typical Type III kerogen. A narrow range of peak Ea distribution indicates relative homogeneity of organic matter which is also evident from FTIR spectra showing relative abundance of aromatic compounds. Maceral assemblage reveals substantial presence of Type I/Type II liptinite macerals namely, alginite, sporinite, cutinite along with Type III vitrinite macerals which likely elevated the kerogen type and hydrogen index (HI), and resulted in a narrow Ea distribution. The kerogen transformation ratio and the hydrocarbon generation rate indicate considerably earlier onset of kerogen transformation and quicker completion of hydrocarbon generation for R4 shales suggesting better potential for R4 shales relative to R1 shales. Furthermore, Rock‐Eval parameters S2, TOC, Hydrogen Index, Tmax summarise that the shales derived predominantly from terrestrial sources contain mainly Type III with some mixed Type II–III kerogen with potential for wet/dry gas generation. In the absence of any post‐depositional igneous activity in the NE part of the Raniganj sub‐basin, the shales are in an early matured state unlike shales from the NW part.
Exploring the role of organofacies in governing kerogen kinetics: A case study of the Permian Gondwana coals from India Monalisa Mallick, Runcie Paul Mathews, Nihar Ranjan Kar, Barnita Banerjee, Subhasmit Dash, E.V.S.S.K. Babu, Srinivas Bikkina, Vikram Partap Singh, Satendra Kumar Gupta, Vireswar Samanta Energy Geoscience, 2026 This study investigates four Late Permian Gondwana coals from the Raniganj sub-basin, Damodar Valley and three Early Permian Gondwana coals from the Talcher sub-basin, Mahanadi Valley. The study aims to characterize the kerogen type, hydrocarbon generation potential, thermal maturity, and organic matter composition, as well as to explore the impact of organic matter characteristics on kerogen kinetic parameters, utilizing multi proxy approach. The study further investigates the influence of the mineral matrix on kerogen decomposition kinetics. Based on the Rock-Eval parameters, Fourier transform infrared spectroscopy (FTIR) parameters, and vitrinite reflectance ( R o ), the kerogen is primarily classified as immature/early mature Type Ⅲ kerogen derived from terrestrial land plants, with minor contribution from Type Ⅱ kerogen having mainly gas generating potential. The source of the organic matter, as determined by stable carbon isotopic composition (δ 13 C org ) values and C/N ratios indicates a primary input from C 3 terrestrial plants. The presence of enriched collotelinites and liptinites, such as sporinite and resinite, provides evidence for the input of terrestrial higher plants, including both herbaceous and arborescent species. Various indices derived from maceral abundances, including the gelification index ( GI ), tissue preservation index ( TPI ), and vegetation index ( VI ), collectively indicate diverse depositional conditions which range from wet forest swamps to shallow water-covered wet forest swamps and even dry forest swamps. The variation in vitrinite macerals influenced the kerogen type and consequently impacted the kinetic parameters, viz. the distribution of activation energies ( E a ), kerogen transformation ratio ( KTR ), and hydrocarbon generation rate ( HGR ). Among the Talcher coals, shaly coals exhibit different kerogen type and kerogen transformation. This dissimilarity can be attributed to variable maceral compositions. Unlike the Talcher samples, all Raniganj samples show consistent kinetic behaviour despite their sample type (coal/shaly coal) or kerogen type (Type Ⅲ/mixed Type Ⅱ/Ⅲ) owing to comparable liptinite/vitrinite maceral composition. This study reveals that whilst the presence of mineral matrix shifts the apparent E a of kerogen through interactions like adsorption and catalysis, it does not significantly affect the kerogen type, HGR , or KTR of the studied coals. • The Permian coals/shaly coals from Raniganj and Talcher sub-basins contain terrestrial Type Ⅲ/Ⅱ kerogen. • E a distribution/FTIR denote heterogeneity of OM. • Organofacies instead of sample nature influences the kerogen type/kinetic parameters. • Different sample nature but similar macerals may exhibit similar kerogen kinetics. • Similar FTIR spectra but different macerals may produce different kinetic outcomes.
Burden of MASLD and liver fibrosis: evidence from Phenome India cohort Meghana Arvind, Anshul Verma, Sreeshma Raj K, Satyartha Prakash, Vignesh S. Kumar, Mohammad Azhar Uddin, Ayushi Narayan, Mamta Rathore, Nancy Rawat, Ankita Sahu, Yogesh Kumar, Pulkit Hasmukhbhai Leuva, Monika Sharma, Rajesh S, Dwaipayan Saha, Ankita Mridha, Ishant Jyoti Nath, Ashique Hussain, Borsha Rajkumari, Mamta Thapa, Neha Kumari, Vishwapriya S, Shilpak Chatterjee, Dipyaman Ganguly, Ashish Awasthi, Vamsi K. Yenamandra, Ajay Pratap Singh, Aastha Mishra, Swasti Raychaudhuri, Karthik Bharadwaj Tallapaka, Giriraj Ratan Chandak, Mahesh J. Kulkarni, Mahesh S. Dharne, Romi Wahengbam, Umakanta Subudhi, Sagnik Biswas, Shalimar, Kumardeep Chaudhary, Shantanu Sengupta, Partha Chakrabarti, Viren Sardana, Abhishek Kumar, Ankit Basnal, Ankur Halder, Anshul Bhardwaj, Ansuman Sahu, Bharti Sharma, Debasis Dash, Deeksha Yadav, Deepak, Kalyani Verma, Komal Jindal, Md. Intyaz Ali, Mohit, Pankaj Pandey, Pranjal Tewari, Pratik Pathade, Praveena Mishra, Rohit Kumar, Ruchi, Safeer Khan, Shail Kumari, Shilpa Ray, Shivani Chitkara, Shubham Kumar, Shyam Singh Bisht, Sumant Kumar, Swarnendu Bag, Swati, Tanmay Pawaskar, Tarani Mathur, Vivek Junghare, Dipamoy Dutta, Jahangir Alam, Pratitusti Basu, Saheli Chowdhury, Saikat Majumder, Dibya Rana Saha Roy, Jukanti Akshitha, M.K. Kanakavalli, Rakhesh KV, Ajit A. Sutar, Ameya A. Pawar, Ankita Namdeo, Apurva Balge, Ashok P. Giri, Chiranjit Chowdhury, Dhanasekaran Shanmugam, Milind Kale, Narendra Y. Kadoo, Nikhilesh Yadav, Rashdajabeen Q. Shaikh, Sagar Baulia, Shivani V. Palkar, Shrutika M. Shewale, Shyam K. Gawari, Syed G. Dastager, Vaishnavi N. Mahajan, Bhabani S. Jena, Boopathy Ramasamy, Sai Adarsh Sahu, Sk Rameej Raja, T Pavan Kumar, Trupti Das, Jagadeshwar Reddy Thota, Prabhakar Sripadi, Ramakrishna Sistla, Ramesh Ummanni, Sai Balaji Andugulapati, Srinivasa Rao M, Adrija Rakshit, Amit Kumar Shahravat, Amit Lahiri, Deepanshu Sindhwani, Kabita Sarkar, Kajal KM, Lakra Promila, Mrigank Srivastava, Rahul Roy, Shail Singh, Shikha Yadav, Smita Pandey, Vivek Bhosale, Gopal Krishna Patra, Iranna Gogeri, Narendra Singh, Raju Khan, Neeraj Jain, Rajesh Kumar Verma, Ganesh Venkatachalam, Murugan Veerapandian, Amit Kumar, Deepak Bansal, Dheeraj Kumar Kharbanda, Dinesh Gupta, Sk. Masiul Islam, Vipul Sharma, Prakash M. Halami, S.P. Muthukumar, Anil Kumar Maurya, Anirban Pal, Daneshvar Prasad, A.K. Raman, Bhanu Pandey, Dikchha Singh, Jai Krishna Pandey, Parimala Karupannan, Suresh Kumar Anandasadagopan, Vandhana Anumaiya, Swati Saha, Vishal Anand, Mukti Advani, Rina Singh, Anamika Kothari, Suman Singh, Avinash Mishra, Pooja Aggarwal, Shreedhar Kanagarjan, Ankita Kumari, Ravi Raj, Vikram Patial, Yogendra Padwad, Fayaz Malik, Kaneez Fatima, Nancy Sharma, Sahaurti Sharma, Sakshi Nagial, Sumit G. Gandhi, Debashish Ghosh, Jyoti Porwal, Pramod Chauhan, Suchismita Benjwal, Neha Mehrotra, Prabhanshu Tripathi, Vikas Srivastava, Amit Tuli, Anshu Bhardwaj, Bhupender Singh, Deepak Sharma, Kuldeep Singh, Lalit Kumar, Parvez Ahmad, Pradip Sen, Pranavathiyani G, Pravin Kumar, Priyadarshan Kinatukara, Priyanshu Singh Raikwar, Rakesh Kumar, Rashmi Kumar, Ritu Jatav, Shiva Sundharam S, Siddhakam Palmal, Simran Gambhir, Srinivasan Krishnamurthi, Abbani Rakesh, Prakash L, Satisha Shri, Indrani Ghosh, Brahma Nanda Singh, Chandana Venkateswara Rao, Madan Mohan Pandey, Sanjeev Kumar Ojha, Vijayanandraj Selvaraj, Prashanti Niwant, Shilpa Paranjape, Manuj Kr Das, Pankaj Bharali, Sukanya Borkakoti, Tridip Phukan, Biswajit Mandal, E.V.S.S.K. Babu, T Vijaya Kumar, Rajeev K. Sukumaran, Rameshkumar N, Bhumika Shirodkar, Kalpana Sandesh Chodankar, Samir Ravikant Damare, Akshika, Arun Uniyal, Arvind Meena, Ansu J. Kailath, K Sudhakara Rao, Krishna Kumar, Kuldeep Singh Gour, Navneet Singh Randhawa, Nikhil Kumar, Priyanka Singh, Roshan Kumar, Arun Kant Singh, Ved Varun Agrawal, Maheswaran Srinivasan, Vasudevan Pandurangan, Manisha Sakpal, Rashmi Arya Lancet Regional Health Southeast Asia, 2026 Background: Metabolic-dysfunction-associated steatotic liver disease (MASLD) is rising globally, including in India, yet community-based data remain scarce. We address this critical knowledge gap by assessing the prevalence, distribution, and characteristics of MASLD subgroups and fibrosis, leveraging the Phenome India cohort. Methods: In this prospective study, we recruited 10,267 adults across 37 laboratories of the Council of Scientific and Industrial Research (CSIR) from 27 Indian cities. All permanent staff members of the CSIR, including current employees, retirees, and their spouses who responded to the recruitment campaign and provided voluntary consent, were considered for participation in the Phenome India Cohort. Steatosis and fibrosis were assessed using Transient Elastography, along with associated clinical, biochemical, cytokine and anthropometric data. Overall, crude and age-adjusted prevalence rates were estimated in the study population and various subgroups. Findings: Of 10,267 individuals screened, 7764 were included, 3712 (47.8%) fulfilled MASLD criteria, corresponding to an age-adjusted prevalence of 38.9% (95% CI 37.2-40.6). Significant fibrosis, defined as liver stiffness measurement (LSM) ≥8.2 kPa (≥F2), was more frequent in MASLD (6.3% [234 of 3688]) than in cases without-MASLD (1.7% [69 of 4027]), corresponding to an age-adjusted prevalence of 4.1% in MASLD. Overall age-adjusted prevalence of significant fibrosis was 2.4%, which clustered in older adults (>60 years) and in those with diabetes or obesity class II, with evidence of possible regional variation. Interpretation: MASLD affected over one-third of participants. Site-specific disparities were observed, which suggest the need for large-scale longitudinal studies to elucidate region-specific risk factors and temporal trends. Community-based awareness and targeted public health interventions across diverse geographical and socio-cultural settings in India may help curb the rising burden. Funding: The work was funded by CSIR, India grant HCP47.
A fresh look at the physicochemical evolution of the lithospheric mantle beneath the Dharwar craton (India) Jiten Pattnaik, Sonja Aulbach, Sujoy Ghosh, E. V. S. S. K. Babu, Fanus Viljoen, Robert Bolhar Mineralogy and Petrology, 2025 The physicochemical evolution of cratonic lithosphere reflects the impacts of tectonomagmatic processes over its lifetime that may be deciphered using kimberlite-borne xenoliths and xenocrysts, but remain poorly constrained for the Indian Dharwar craton, owing to the dearth of fresh mantle material. This study examines detailed petrography and geochemical composition of six eclogite xenoliths, and additional eclogitic and peridotitic garnet separates, from the Wajrakarur kimberlites in the Eastern Dharwar Craton (EDC). Clinopyroxene in eclogite xenoliths is too altered to permit contamination-free sampling during laser ablation for trace element analysis. We overcome this limitation by exploiting relationships of clinopyroxene-garnet distribution coefficients with garnet Ca#, clinopyroxene jadeite content, and temperature. This allows a more accurate delineation of their petrogenesis from reconstructed bulk rocks and indicates their origin from variably plagioclase-rich oceanic crustal protoliths, with weak subsequent metasomatic overprint. In contrast, estimates of Fe³⁺ in garnet from peridotite xenoliths indicate an oxygen fugacity shift towards more oxidized conditions beneath the EDC linked to enrichment in melt-mobile elements (Ti, Zr) in the barren or weakly diamondiferous P1 and P3 kimberlites. The most depleted and reduced sample [ΔlogfO2 (FMQ) of -4.3; where FMQ corresponds to the fayalite-quartz-magnetite buffer] derives from diamondiferous kimberlite P7, suggesting oxidative melt metasomatism as a key control on the regional diamond inventory, although more data are needed. EDC eclogites and peridotites have estimated P-wave velocities of 8.46–8.63 km/s and 8.21–8.22 km/s, respectively, which are lower than present-day observed bulk P-wave velocities, and may point to lithological or thermal changes since Mesoproterozoic entrainment.
Holocene climate variability deciphered from Chilika Lagoon sediments: Implication for anthropogenic activity or paleocyclones? Barnita Banerjee, Monalisa Mallick, Mohd Amir, Abdul Hameed, Luan Ozelim, Nihar Ranjan Kar, E.V.S.S.K. Babu, K. Venkatesham, M. Venkateshwarlu, Tanveer Hassan, Vireswar Samanta, Prem Chand Kisku, Debajyoti Paul, Pankaj Kumar, Aurovinda Panda Geosystems and Geoenvironment, 2025 • High energy event post ∼1.1 Ka is recorded in the lacustrine sediments of Chilika. • Indian summer monsoon was high during the early Holocene. • CaCO 3 content and F2 values suggest the formation of barrier spit post ∼4 Ka. • High physical weathering dominated during ∼4 Ka arid period. Coastal lagoons, acting as a link between land and sea, serve as valuable archives for past climate variations, human activities, and paleo-cyclonic events. In this study, we employ a multi-proxy approach to analyze sedimentary records and uncover climatic shifts influenced by both monsoonal and non-monsoonal factors. Our analysis incorporates sediment characteristics such as grain size, magnetic susceptibility (MS), and clay mineralogy to infer high-energy conditions within the Chilika Lagoon. Additionally, we utilize Rock-Eval pyrolysis and deconvolution of flame ionization detector (FID) signals to determine the type of organic matter (OM) present. Findings reveal that during the Early Holocene, a high sand percentage and elevated MS indicate an intensified monsoon, coinciding with a dominance of terrestrial OM. However, as monsoonal intensity declined after the Early Holocene, marine OM became more prevalent, likely linked to the formation of an estuary around ∼7.7 Ka. Despite a weakening monsoon around ∼4 Ka, MS values remained high, possibly due to increased aeolian input, which transported titanomagnetite, contributing to elevated MS in the sediment record. After ∼4 Ka, the sedimentary record indicates a greater influx of terrestrial OM, likely due to the formation of a barrier spit that limited marine influence. From this period onward, monsoonal intensity gradually increased, peaking around ∼1.1 Ka, coinciding with the Medieval Warm Period. Following ∼1.1 Ka, sedimentation rates rose, accompanied by low magnetic susceptibility (MS) and high sand content. This phase also shows an increase in both terrestrial and marine OM, along with higher CaCO₃ and illite concentrations, suggesting the impact of high-energy events, possibly cyclones. The intensification of cyclonic activity after ∼1.1 Ka may be associated with a weakening of El Niño–Southern Oscillation (ENSO) intensity during this period.
Petromineragraphy and mineral chemistry of bituminous shale-hosted uranium mineralisation at Sonrai, Lalitpur District, Uttar Pradesh Journal of the Geological Society of India, 2004
Petrography, mineral chemistry and geothermobarometry of the Inukurti Anorthosite Complex and associated rocks from the Nellore Schist Belt, Andhra Pradesh Journal of the Geological Society of India, 2003
REE geochemistry of the Uranium phases in syn-magmatic and hydrothermal-type u-mineralisation: Two case histories from India Journal of the Geological Society of India, 2003
X-ray powder diffractometry and electron microprobe study of partially disordered wodginites from Challanpara pegmatite, Bastar District, Chattisgarh Journal of the Geological Society of India, 2002
Uranium mineralisation in the Neoproterozoic Bhima basin at Gogi and near Ukinal: An ore petrological study Journal of the Geological Society of India, 2002
Discrete selenide phases from the uraniferous Mahadek sandstones of Domiasiat and Wahkyn South, West Khasi Hills District, Meghalaya Journal of the Geological Society of India, 2002
Chemistry of eclogitic garnets from Bahradih kimberlite, Raipur district, Madhya Pradesh Journal of the Geological Society of India, 2000
Compositional study of spinels from Wajrakarur Pipe-10 (Anumpalle), Ananthapur district and its significance in diamond prospectivity Journal of the Geological Society of India, 1998
Cluster analysis and nickel thermometry of garnet xenocrysts from Majhgawan diamondiferous pipe, Panna District, Madhya Pradesh Journal of the Geological Society of India, 1998
Spinel (hercynite) adcumulate from the Chimakurti gabbro-anorthosite pluton, Prakasam District, Andhra Pradesh, India: Evidence for plagioclase buoyancy and magma mixing Current Science, 1997
Fossil pigeonites and exsolution features in pyroxenes from ferrosyenites of south India Journal Geological Society of India, 1993
RECENT SCHOLAR PUBLICATIONS
Geochronology, mineralogy, and Trace and Rare Earth Element Geochemistry of the Dargawan Sill, Bijawar Basin, India: Implications for Magma Genesis PS Sangita, M Ovtcharova, TV Kumar, A Bekker, G Balu, E Babu, ... Goldschmidt 2026 Conference , 2026 2026
Authigenic carbonate crust archives a protracted seepage event of deep-seated methane sources M Sadique, A Mazumdar, A Peketi, A Hasozbek, TV Kumar, E Babu, ... Chemical Geology, 123416 , 2026 2026
Permian Carbonaceous Shales From Raniganj Sub‐Basin—A Potential Source of Hydrocarbons? Inferences Drawn From Kerogen Characteristics and Kinetics M Mallick, B Banerjee, NR Kar, RP Mathews, VP Singh, M Tiwari, E Babu, ... Geological Journal 61 (4), 1143-1166 , 2026 2026 Citations: 2
Burden of MASLD and liver fibrosis: evidence from Phenome India cohort M Arvind, A Verma, S Prakash, VS Kumar, MA Uddin, A Narayan, ... The Lancet Regional Health-Southeast Asia 45 , 2026 2026 Citations: 4
Magnetic mineralogical and sedimentological approach for tracing source-to-sink processes in a tropical fluvial, estuarine, and marine system F Badesab, N Kadam, P Pednekar, S Shaheen, O Sagavekar, S Gullapalli, ... Continental Shelf Research, 105630 , 2025 2025
Exploring the role of organofacies in governing kerogen kinetics: A case study of the Permian Gondwana coals from India M Mallick, RP Mathews, NR Kar, B Banerjee, S Dash, E Babu, S Bikkina, ... Energy Geoscience, 100503 , 2025 2025 Citations: 1
A 125 years (1879–2003 CE) record of seasonal δ18O changes in a Porites lutea coral from the Lakshadweep Archipelago, southeastern Arabian Sea W Raza, SM Ahmad, SK Beja, CY Huang, CC Shen, E Babu Journal of Marine Systems, 104142 , 2025 2025
Petrology and Geochemistry of Poikilitic Shergottite Northwest Africa 1950: bridging the gap between depleted and intermediate sources in Martian Mantle VM Nair, AB Sarbadhikari, GNSS Bhuvan, TV Kumar, N Sorcar, ... Geochimica et Cosmochimica Acta , 2025 2025 Citations: 1
Paleo-productivity reconstruction in Bay of Bengal during the past 1.3 Ma: Implications for glacial-interglacial dynamics and southern hemispheric processes B Banerjee, M Mallick, V Kumar, E Babu, O Luan, G Balu, TV Kumar, ... Palaeogeography, Palaeoclimatology, Palaeoecology 672, 113004 , 2025 2025 Citations: 1
PETROLOGY AND GEOCHEMISTRY OF POIKILITIC SHERGOTTITE NWA 1950: INSIGHTS INTO MARTIAN MANTLE SOURCES VM Nair, AB Sarbadhikari, GNS Bhuvan, TV Kumar, N Sorcar, ... METEORITICS & PLANETARY SCIENCE 60 , 2025 2025
Holocene climate variability deciphered from Chilika Lagoon sediments: Implication for anthropogenic activity or paleocyclones? B Banerjee, M Mallick, M Amir, A Hameed, L Ozelim, NR Kar, E Babu, ... Geosystems and Geoenvironment 4 (3), 100390 , 2025 2025 Citations: 2
A fresh look at the physicochemical evolution of the lithospheric mantle beneath the Dharwar craton (India) J Pattnaik, S Aulbach, S Ghosh, EVSSK Babu, F Viljoen, R Bolhar Mineralogy and Petrology 710 (025), 00943 , 2025 2025 Citations: 3
Chemical tomography of Dharwar SCLM: Insights from equilibrium olivine composition from Kimberlite-borne clinopyroxene xenocrysts S Dash, E Babu Authorea Preprints , 2025 2025
Source Rock Properties, Depositional Environment and Kerogen Degradation Kinetics of Lower Permian Shales from the Ib River Sub‐Basin, Mahanadi Basin, Eastern India NR Kar, D Mani Tiwari, J Buragohain, B Hazra, E Babu, BS Seetha, ... Journal of Petroleum Geology 48 (2), 85-110 , 2025 2025
Plate tectonics through Earth’s history: constraints from the thermal evolution of Earth’s upper mantle S Dash, E Babu, J Ganne, S Mukherjee International Geology Review 67 (4), 500-533 , 2025 2025 Citations: 8
Organic provenance and depositional environment of Eocene carbonaceous rocks from petroliferous Barmer basin, Western Rajasthan, India NR Kar, D Mani, BS Seetha, B EVSSK, S Mukherjee, S Dasgupta, ... Journal of the Geological Society of India 101 (1), 112-122 , 2025 2025 Citations: 2
Biomarker evidence of shifts in organic provenance and depositional environments of Eocene carbonaceous rocks from petroliferous Barmer basin, western Rajasthan, India NR Kar, D Mani, BS Seetha, E Babu, S Mukherjee, S Dasgupta, ... Journal of the Geological Society of India 101 (1), 112-122 , 2025 2025 Citations: 11
Reconstruction of weathering history and paleoclimatic conditions of the campano-maastrichtian sandstones in The Northern Bida Basin, Nigeria SA Adepoju, OJ Ojo, SO Akande, B Sreenivas, E Babu, TV Kumar Discover Geoscience 2 (1), 102 , 2024 2024 Citations: 1
Tracing the late permian Gondwana surface environments using sedimentary biomarkers from the Raniganj Formation, Damodar Valley, Eastern India NR Kar, D Mani, E Babu Journal of Sedimentary Environments 9 (4), 813-836 , 2024 2024 Citations: 4
An evaluation of glass beads from the southwestern coastal state of Goa, India, as a potential pollutant in marine ecosystem NG Rudraswami, VP Singh, M Pandey, E Babu, TV Kumar Environmental Monitoring and Assessment 196 (11), 1127 , 2024 2024 Citations: 2
MOST CITED SCHOLAR PUBLICATIONS
In situ FTIR study on the dehydration of natural goethite PSR Prasad, K Shiva Prasad, V Krishna Chaitanya, E Babu, B Sreedhar, ... Journal of Asian Earth Sciences 27 (4), 503-511 , 2006 2006 Citations: 207
A translithospheric suture in the vanished 1-Ga lithospheric root of South India: evidence from contrasting lithosphere sections in the Dharwar Craton WL Griffin, AF Kobussen, E Babu, SY O'Reilly, R Norris, P Sengupta Lithos 112, 1109-1119 , 2009 2009 Citations: 109
Phase relations of osumilite and dehydration melting in pelitic rocks: a simple thermodynamic model for the KFMASH system TJB Holland, E Babu, DJ Waters Contributions to Mineralogy and Petrology 124 (3), 383-394 , 1996 1996 Citations: 91
A new cache of Eoarchaean detrital zircons from the Singhbhum craton, eastern India and constraints on early Earth geodynamics B Sreenivas, S Dey, YJB Rao, TV Kumar, E Babu, IS Williams Geoscience Frontiers 10 (4), 1359-1370 , 2019 2019 Citations: 90
Zircon U-Pb ages and Hf isotopic systematics of charnockite gneisses from the Ediacaran–Cambrian high-grade metamorphic terranes, southern India: Constraints on crust formation … TV Kumar, YJB Rao, D Plavsa, AS Collins, JK Tomson, BV Gopal, E Babu Bulletin 129 (5-6), 625-648 , 2017 2017 Citations: 52
Uranium mineralisation in the Neoproterozoic Bhima Basin at Gogi and near Ukinal: an ore petrological study RD Raju, MK Kumar, E Babu, SA Pandit Journal of the Geological Society of India 59 (4), 299-321 , 2002 2002 Citations: 50
Evidence for Neoarchean basement for the Deccan volcanic flows around Koyna-Warna region, western India: Zircon U-Pb age and Hf-isotopic results YJB Rao, B Sreenivas, TV Kumar, N Khadke, AK Krishna, E Babu Journal of the Geological Society of India 90 (6), 752-760 , 2017 2017 Citations: 45
Source rock properties and kerogen decomposition kinetics of Eocene shales from petroliferous Barmer basin, western Rajasthan, India NR Kar, D Mani, S Mukherjee, S Dasgupta, MK Puniya, AK Kaushik, ... Journal of Natural Gas Science and Engineering 100, 104497 , 2022 2022 Citations: 41
Fractionation and fragmentation of glass cosmic spherules during atmospheric entry NG Rudraswami, MS Prasad, E Babu, TV Kumar, W Feng, JMC Plane Geochimica et Cosmochimica Acta 99, 110-127 , 2012 2012 Citations: 41
Grain to outcrop-scale frozen moments of dynamic magma mixing in the syenite magma chamber, Yelagiri Alkaline Complex, South India ML Renjith, SN Charan, DV Subbarao, E Babu, VB Rajashekhar Geoscience Frontiers 5 (6), 801-820 , 2014 2014 Citations: 39
Insights from a Pan India sero-epidemiological survey (phenome-India cohort) for SARS-CoV2 S Naushin, V Sardana, R Ujjainiya, N Bhatheja, R Kutum, AK Bhaskar, ... Elife 10, e66537 , 2021 2021 Citations: 38
Zircon U–Pb and molybdenite Re–Os geochronology, with S isotopic composition of sulfides from the Chah-Firouzeh porphyry Cu deposit, Kerman Cenozoic arc, SE Iran H Mohammaddoost, M Ghaderi, TV Kumar, J Hassanzadeh, S Alirezaei, ... Ore Geology Reviews 88, 384-399 , 2017 2017 Citations: 33
Correlation of the oldest Toba Tuff to sediments in the central Indian Ocean Basin JN Pattan, M Shyam Prasad, E Babu Journal of Earth System Science 119 (4), 531-539 , 2010 2010 Citations: 33
Chemical, isotopic and amino acid composition of Mukundpura CM2. 0 (CM1) chondrite: Evidence of parent body aqueous alteration NG Rudraswami, AK Naik, RP Tripathi, N Bhandari, SG Karapurkar, ... Geoscience Frontiers 10 (2), 495-504 , 2019 2019 Citations: 31
A Review of Paleo-to Neoarchean crustal evolution in the Dharwar craton, Southern India and the transition towards a Plate Tectonic regime YJB Rao, TV Kumar, B Sreenivas, E Babu Episodes Journal of International Geoscience 43 (1), 51-68 , 2020 2020 Citations: 30
Geochemistry and isotopic study of southern Bay of Bengal sediments: Implications for provenance and paleoenvironment during the middle Miocene B Banerjee, S Masood Ahmad, EVSSK Babu, VM Padmakumari, ... Paleogeography, Paleoclimatology, Paleoecology 514, 156-167 , 2019 2019 Citations: 27
Martian meteorite Tissint records unique petrogenesis among the depleted shergottites A Basu Sarbadhikari, E Babu, T Vijaya Kumar, H Chennaoui Aoudjehane Meteoritics & Planetary Science 51 (9), 1588-1610 , 2016 2016 Citations: 27
Chemistry and petrology of Fe–Ni beads from different types of cosmic spherules: Implication for precursors NG Rudraswami, MS Prasad, E Babu, TV Kumar Geochimica et Cosmochimica Acta 145, 139-158 , 2014 2014 Citations: 26
Ordinary chondritic micrometeorites from the Indian Ocean MS Prasad, NG Rudraswami, A De Araujo, E Babu, T Vijaya Kumar Meteoritics & Planetary Science 50 (6), 1013-1031 , 2015 2015 Citations: 22
Origin of Cretaceous phosphorites from the onshore of Tamil Nadu, India V Purnachandra Rao, PM Kessarkar, R Nagendra, E Babu Journal of earth system science 116 (6), 525-536 , 2007 2007 Citations: 21