Are earthquake swarms in South Gujarat, northwestern Deccan Volcanic Province of India monsoon induced?

South Gujarat, a part of the northwestern Deccan Volcanic Province of India has been experiencing episodic swarm activity with reports of sounds, whose association remains unclear. After the Indian monsoon period, during the month of September 2016, a swarm activity occurred around the Keliya dam in...

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Bibliographic Details
Published in:	Environmental earth sciences 2019-07, Vol.78 (13), p.1-13, Article 381
Main Authors:	Sateesh, A., Mahesh, P., Singh, A. P., Kumar, Santosh, Chopra, Sumer, Kumar, M. Ravi
Format:	Article
Language:	eng
Subjects:	Acoustics Annual rainfall Biogeosciences Blasting Earth and Environmental Science Earth Sciences Earthquakes Environmental Science and Engineering Frequency ranges Geochemistry Geological faults Geology Hydrology/Water Resources Mean annual precipitation Monsoons Original Article Rain Rainfall Seismic activity Seismicity Strike-slip faults Summer monsoon Terrestrial Pollution Trends Wind
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Summary:	South Gujarat, a part of the northwestern Deccan Volcanic Province of India has been experiencing episodic swarm activity with reports of sounds, whose association remains unclear. After the Indian monsoon period, during the month of September 2016, a swarm activity occurred around the Keliya dam in the Navsari district of South Gujarat and nearby villages in the Dadra and Nagar Haveli (DNH), which continued for about 4 months. Again, the swarm activity recurred during the month of August 2017 and continued for about 5 months till January 2018. Many of these events were accompanied by audible sounds, like blasting, that caused severe panic among local occupants. A local network of four stations was installed to monitor the swarm activity, in addition to the Gujarat state seismic network. A total of 1048 earthquakes were located around the Keliya dam and 229 events in the DNH region from September 2016 to June 2018. In the present study, we performed a spectrogram analysis of the events with associated sounds. The analysis revealed significant energy at frequencies ≥ 20 Hz, in the audible frequency range. The relocated earthquake distribution shows that seismicity in the Navsari district follows a ~ NW–SE trend, confined to an area of 13 km × 2 km with a depth extent of 3 km. The trend is similar in the DNH region, confined to an area of 15 km × 2 km, down to a depth of 6 km. The determined focal mechanism in DNH region shows strike-slip faulting. The seismicity patterns seem to corroborate with the trends of the lineaments/dykes in the region. In general, the swarm-type earthquake sequences seem to occur when the annual rainfall exceeds the mean annual rainfall. We speculate that the present swarm activity, noticed with some delay after the Indian summer monsoon season, may be due to the phenomenon of hydro-seismicity.
ISSN:	1866-6280 1866-6299