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Kundu, Bhaskar, Vissa, Naresh Krishna, and Gahalaut, V. K., 2015. Influence of anthropogenic groundwater unloading in Indo-Gangetic plains on the 25 April 2015 Mw 7.8 Gorkha, Nepal earthquake. Geophysical Research Letters, 42(24):10,607–10,613, doi:10.1002/2015GL066616.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2015GeoRL..4210607K,
author = {{Kundu}, Bhaskar and {Vissa}, Naresh Krishna and {Gahalaut}, V.~K.},
title = "{Influence of anthropogenic groundwater unloading in Indo-Gangetic plains on the 25 April 2015 Mw 7.8 Gorkha, Nepal earthquake}",
journal = {\grl},
keywords = {2015 Gorkha, Nepal earthquake, Indo-Gangetic plains, groundwater, Nepal Himalaya, Coulomb stress, Main Himalayan Thrust},
year = 2015,
month = dec,
volume = {42},
number = {24},
pages = {10,607-10,613},
abstract = "{Groundwater usage in the Indo-Gangetic plains exceeds replenishment of
aquifers, leading to substantial reduction in the mass. Such
anthropogenic crustal unloading may promote long-term fault slip
or may modulate seismic activity in the adjoining Himalayan
region. Our simulation using Gravity Recovery and Climate
Experiment data and hydrological models of such a process
indicates that the thrust earthquakes on the Main Himalayan
Thrust (MHT), including the recent 25 April 2015 Mw 7.8 Gorkha,
Nepal earthquake, are probably influenced by the anthropogenic
groundwater unloading process in the Gangetic plains. The
groundwater withdrawal leading to crustal unloading in the
Gangetic plains causes a significant component of horizontal
compression which adds to the secular interseimic compression at
the seismogenic depth (5-20 km) on the MHT beneath the Himalayan
arc and at hypocentral depth of the 2015 Gorkha, Nepal
earthquake. This effect enhances the Coulomb stress on the
locked zone of MHT.}",
doi = {10.1002/2015GL066616},
adsurl = {https://ui.adsabs.harvard.edu/abs/2015GeoRL..4210607K},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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