The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

Since its deployment at the surface of Mars, the Seismic Experiment for Interior Structure
(SEIS) instrument of the InSight mission has detected hundreds of small‐magnitude seismic …

Abstract We review Reservoir Triggered Seismicity (RTS) in the Koyna-Warna region of
India since the impoundment of the Koyna reservoir in 1962 until the year 2015. We include …

The attenuation of seismic wave energy in NW Himalayas has been estimated using local
earthquakes. Most of the analyzed events are from the vicinity of the Main Boundary Thrust …

Complementing a series of recent seismic hazard studies for Hong Kong, we have estimated
the Q factor using 25 local earthquakes, within 200 km of Hong Kong, digitally recorded from …

During the later half of the twentieth century, seismic instrumentation had seen rapid growth,
enabling generation of very useful data sets not only for unravelling the very important …

The attenuation properties of the crust in the Kachchh region, Gujarat, India, have been
investigated. For this purpose, 49 local earthquakes having focal depths in the 3–38 km …

In this study, the attenuation of coda waves Q c (f) has been estimated for different lapse
times and frequencies in the East Anatolian Fault Zone (EAFZ) in Turkey using a single back …

The attenuation of coda waves, Q c, has been estimated in Zarand, Jiroft, and Bam regions
of east central Iran using a single back-scattering model of S-coda envelopes. For this …

High-frequency strong-motion data of two recent major earthquakes of the Garhwal
Himalayan region of India have been analyzed to determine the Qβ (f) for this region. Data …