Shashidhar D, Mahesh P, Gupta S, Mallika K.
SEISMOLOGICAL RESEARCH LETTERS
https://doi.org/10.1785/0220250319
Data from 5325 local earthquakes recorded on eight deep borehole seismic sensors to generate a sub-basalt velocity model for the Koyna Reservoir region, India. For the first time, the VP and Vp/Vs images reveal strong lateral and vertical heterogeneity within the granitic basement, with distinct velocity anomalies across the Donachiwada fault (DF) at 6-10km depth, coinciding with a dense cluster of seismicity. DF is the plausible source of the 10 December 1967 (M 6.3) earthquake - the largest reservoir-triggered event documented globally.
Cross sections across the DF of (a) P-wave velocity and (b) VP=VS. The dashed line (white) indicates the presence of DF at depths.
Permanent borehole seismic stations and seismicity at the Koyna Warna region, western India.