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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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發(fā)表于 2025-3-21 18:29:58 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Microearthquake Seismology and Seismotectonics of South Asia
編輯J. R. Kayal
視頻videohttp://file.papertrans.cn/634/633180/633180.mp4
概述Covers topics ranging from basics of plate tectonics, seismology, data acquisition, seismogram analysis to use of software for earthquake locations, relocations, fault plane solutions, seismic tomogra
圖書(shū)封面Titlebook: Microearthquake Seismology and Seismotectonics of South Asia;  J. R. Kayal Book 2008 Capital Publishing Company, New Delhi, India 2008 Eart
描述Hardly a week passes without our learning of natural geologic disaster somewhere in the world, be it a volcanic eruption, landslide, or destructive earthquake. The prominent public notice given to such events is not only the result of better communications, but also results from the increased impact of these events on a growing human population. In recent years, the population has increased greatly in regions of active tectonics. Northern India and the surrounding areas are prime examples. The consequence is that people and their man-made structures are concentrated close to active faults and steep, landslide-prone terrains. In just the past several years, even moderate earthquakes with seismic magnitudes less than 6. 5 have killed as many as 20,000 people precisely because these earthquakes occurred directly beneath population centres in central India. The greater Himalayan region, including the Ganges Plain, is a prime example of the coexistence of a pronounced geological hazard with a growing human population. Due in part to the spectacular topography, the region has long attracted scientific investigations, and may be considered as the birthplace of modern studies of earthquake
出版日期Book 2008
關(guān)鍵詞Earthquakes and tsunamis; Geoinformationssysteme; Himalaya; Microearthquake seismology; Seismotectonics;
版次1
doihttps://doi.org/10.1007/978-1-4020-8180-4
isbn_softcover978-90-481-7795-0
isbn_ebook978-1-4020-8180-4
copyrightCapital Publishing Company, New Delhi, India 2008
The information of publication is updating

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Seismotectonics of Peninsular India and Sri Lanka,ar is known as a stable cratonic subcontinent. It was reported that the seismicity of peninsular India is low (Chandra, 1977), despite its ongoing collision with central Asia (Tapponnier et al., 1986). During the last decade (1993–2003), however, three strong/large earthquakes (M 6.0≈7.7) occurred in peninsular India (Fig. 7.2).
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Book 2008rthquake. The prominent public notice given to such events is not only the result of better communications, but also results from the increased impact of these events on a growing human population. In recent years, the population has increased greatly in regions of active tectonics. Northern India a
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Earthquakes and Seismic Waves,ents a problem of explanation and interpretation of every wriggle of the seismic waves produced by the earthquakes. Earthquake seismology is thus defined to be a dual science, a border line field between geology and geophysics. It calls for sound physical and mathematical thinking, and a strong background of geological concepts.
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Northeast India, Myanmar, Bangladesh and Andaman-Sumatra Region,ion (e.g. Mitchell, 1981; Curray et al., 1979 and 1982). Several contrasting views are put forward concerning the seismotectonics of northeast India. Uyeda and Kanamori (1979) postulated that the Alpine-Himalayan orogenic belt and the Andaman-Indonesian mobile belt are linked by a transform fault, a
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