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Titlebook: Microearthquake Seismology and Seismotectonics of South Asia; J. R. Kayal Book 2008 Capital Publishing Company, New Delhi, India 2008 Eart

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Introduction, them. The sources can be natural earthquakes or man-made sources of deformational energy that generate the seismic waves. Study of the seismic waves of the Earth provides the highest resolution of the internal Earth structure that no other geophysical method can provide. It is a branch of geophysic
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Earthquakes and Seismic Waves,f man, or breaks up and changes the ground surfaces. To the engineers, the earthquakes of great interest are those which affect the stability and safety of the buildings and other constructions. To the geologists, the earthquake phenomena of interest are the evidence of faulting or other tectonic pr
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Microearthquake Recording and Data Analysis,es in various parts of India. Although this work also had important beginnings at the NGRI (National Geophysical Research Institute), IMD (India Meteorological Department), University of Roorkee (presently Indian Institute of Technology, Roorkee), WIHG (Wadia Institute of Himalayan Geology) and at t
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Dynamics of Faulting and Fault Plane Solution,ss of . accumulation and the triggering mechanism are the basics to understand the earthquake kinematics. The term . or . conventionally refers to fault orientation, the displacement and stress release patterns and the dynamic process of seismic wave generation.
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Himalayas, Pamir-Hindu Kush and Foredeep Region,968; McKenzie and Sclater, 1971; Bowin, 1973; Sclater and Fisher, 1974; Johnson et al., 1976; Curray et al., 1982; Powell et al., 1980). The Indian plate travelled north and north-eastward in between the Ninety East Ridge and Chagos-Laccedive transform fault during Cenozoic (Gansser, 1966), (Fig. 5.
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sed, and spent time with family shifted. Changes in nearly every aspect of daily life became the norm with no time to adapt. Face-to-face appointments were swapped for online consultations, face masks and physical distancing requirements were standard, and nuanced social interactions changed. People
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