Journal of the Geological Society of India

Papers
(The H4-Index of Journal of the Geological Society of India is 14. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-11-01 to 2024-11-01.)
ArticleCitations
Prediction of Flood in Barak River using Hybrid Machine Learning Approaches: A Case Study43
A Perspective on Rishiganga-Dhauliganga Flash Flood in the Nanda Devi Biosphere Reserve, Garhwal Himalaya, India36
Assessment of Flood Frequency using Statistical and Hybrid Neural Network Method: Mahanadi River Basin, India34
AHP and TOPSIS Based Sub-Watershed Prioritization and Tectonic Analysis of Ami River Basin, Uttar Pradesh27
Geomorphic Analysis, Morphometric-based Prioritization and Tectonic Implications in Chite Lui River, Northeast India26
Hydrogeochemical Processes Regulating the Groundwater Quality and its Suitability for Drinking and Irrigation Purpose in Parts of Coastal Sindhudurg District, Maharashtra25
Fluoride Hazard and Risk Enumeration of Hard Rock Unconfined Aquifers in the Extended Part of Chhota Nagpur Gneissic Complex23
Quantitative Morphometric and Morphotectonic Analysis of Pahuj Catchment Basin, Central India20
An Integrated Approach for Delineating and Characterizing Groundwater Depletion Hotspots in a Coastal State of India19
Estimation of Soil Erosion Using RUSLE Model and GIS Tools: A Study of Chilika Lake, Odisha16
Reliability Analysis for Liquefaction Risk Assessment for the City of Patna, India using Hybrid Computational Modeling15
Shock Metamorphic Features in the Archean Simlipal Complex, Singhbhum Craton, Eastern India: Possible Remnant of a Large Impact Structure15
Earthquake Early Warning Systems in Taiwan: Current Status15
Rare Earth Element Deposits: Sources, and Exploration Strategies14
Hydrological Characteristics of 7th February 2021 Rishi Ganga Flood: Implication towards Understanding Flood Hazards in Higher Himalaya14
0.039101123809814