@COMMENT This file was generated by bib2html_grace.pl <https://sourceforge.net/projects/bib2html/> version 0.94
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@ARTICLE{2025AcGeo..73.3431A,
       author = {{Aruna Kumari}, Kondarathi and {Surinaidu}, Lagudu and {Srinu}, Yedavally and {Gahalaut}, Kalpna},
        title = "{Geological heterogeneity and hydrological dynamics impact on triggered earthquake genesis in Deccan basaltic terrain of western India}",
      journal = {Acta Geophysica},
     keywords = {Koyna-Warna reservoirs, Triggered earthquakes, Geospatial techniques, Lineament density, Lineament trend, Groundwater storage anomaly},
         year = 2025,
        month = aug,
       volume = {73},
       number = {4},
        pages = {3431-3440},
     abstract = "{Reservoir triggered seismicity (RTS) have been documented at about 700
        locations worldwide, with the Koyna-Warna region in Western
        India hosted the largest triggered earthquake of magnitude 6.3.
        Despite substantial work has been done to understand the genesis
        of triggered earthquakes around Koyna-Warna reservoirs, most of
        the research has been limited to the immediate areas of the
        reservoirs. In this study, we expand the investigation to
        encompass a broader area, aiming to explore the impact of
        geological heterogeneity and groundwater storage anomalies
        derived from GRACE satellite data on earthquake occurrence in
        the region. Utilising 30-m resolution digital elevation model,
        we extracted lineaments and generated lineament density and
        trend maps. Analysis reveals a total of 927 lineaments spanning
        33.73 km, with shorter lineaments comprising 70\% of the total
        count. Lineament density ranges from 0 to 1.8 km/km$^{2}$,
        indicating varying degrees of rock fracturing, with densities of
        0.6-1.20 km/km$^{2}$ and 0.4-0.6 km/km$^{2}$ indicate high and
        moderate levels. Dominant lineament trends are observed in the
        N-S, NNW-SSE and WNW-ESE directions. Good correlation between
        lineament density, and earthquake occurrence is observed which
        is further validated from groundwater anomaly.}",
          doi = {10.1007/s11600-025-01604-7},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025AcGeo..73.3431A},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
