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Influence of anthropogenic groundwater pumping on the 2017 November 12 M7.3 Iran-Iraq border earthquake

Kundu, Bhaskar, Vissa, Naresh Krishna, Gahalaut, Kalpna, Gahalaut, Vineet Kumar, Panda, Dibyashakti, and Malik, Kapil, 2019. Influence of anthropogenic groundwater pumping on the 2017 November 12 M7.3 Iran-Iraq border earthquake. Geophysical Journal International, 218(2):833–839, doi:10.1093/gji/ggz195.

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@ARTICLE{2019GeoJI.218..833K,
       author = {{Kundu}, Bhaskar and {Vissa}, Naresh Krishna and {Gahalaut}, Kalpna and {Gahalaut}, Vineet Kumar and {Panda}, Dibyashakti and {Malik}, Kapil},
        title = "{Influence of anthropogenic groundwater pumping on the 2017 November 12 M7.3 Iran-Iraq border earthquake}",
      journal = {Geophysical Journal International},
     keywords = {Loading of the Earth, Satellite geodesy, Earthquake dynamics, Induced seismicity, Continental tectonics: compressional},
         year = 2019,
        month = aug,
       volume = {218},
       number = {2},
        pages = {833-839},
     abstract = "{Study of induced, triggered, stimulated and nuance earthquakes can
        provide a unique opportunity to probe into stress/frictional
        conditions on the subsurface fault. Although mechanism of
        faulting is tectonically driven phenomenon, anthropogenic
        crustal (un-)loading process can also drive long-term fault slip
        or modulate seismicity in the nearby seismogenic crust. Using
        Gravity Recovery and Climate Experiment data, surface subsidence
        rate captured by cGPS and 3-D hydrological stress models, we
        report that the 2017 November 12 M7.3 Iran-Iraq border
        earthquake in the Arabia-Eurasia collision boundary region of
        the Zagros fold-and-thrust belt was significantly influenced by
        the anthropogenic groundwater unloading in the Euphrates and
        Tigris River plains and western Iran, a region which is probably
        the most intensely irrigated region in the Middle East. We find
        that the anthropogenic crustal unloading contributed about one
        tenth of the secular interseismic stress change rate due to
        tectonic loading. Thus, the resulting cumulative stress
        accumulation was significantly influenced by the extensive
        groundwater pumping.}",
          doi = {10.1093/gji/ggz195},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2019GeoJI.218..833K},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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