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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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HISTORICAL SEISMICITY AND EARTHQUAKECATALOGUES FOR THE INDIAN REGIONH. N. Srivastava and S. K. DasIndia Meteorological DepartmentLo& Road, New Delhi - 110009, IndiaABSTRACTSeismicity of <strong>the</strong> Indian region is discussed in <strong>the</strong> light of <strong>the</strong> historicaldata vis a vis expansion of seismological network in <strong>the</strong> country. Thesources of epicentral data for this region are based on monthly seismologicalbulletins prepared by <strong>the</strong> India Meteorological Department, U.S.Geological Survey and International Seismological Centre, and cataloguesof earthquakes by Tandon and Srivastava (1974) and many o<strong>the</strong>rs. Thelimitations of <strong>the</strong>se catalogues are discussed. The utility of a new catalogueof earthquakes in peninsular India for <strong>the</strong> period 1849 to 1900,based on felt reports through three newspapers (Times of India, Statesmanand Hindu) is briefly discussed. This catalogue has brought out someinteresting results. In particular, it has been noticed that in <strong>the</strong> regionwhere significant earthquakes have occurred, tremors of felt intensity havebeen reported several years preceding <strong>the</strong> main events. Recently, earthquakesof similar intensity, as reported in <strong>the</strong> catalogue, have occurrednear Hyderabad (30 June 1983; magnitude 4.8) and Bangalore (20 March1985; magnitude 4.5) showing its utility in assessment of earthquake risk.The India Meteorological Department is participating in <strong>the</strong> IASPEI<strong>Historical</strong> Seismogram Filming Project and more than 20,000 seismogramsof Bombay have been microfilmed during <strong>the</strong> last two years. The recenttechniques of source mechanism studies through digitieation of old records(prior to 1962), as envisaged in <strong>the</strong> TASPEI <strong>Historical</strong> Seismogram FilmingProject, will enable us to understand <strong>the</strong> nature of stresses in andaround <strong>the</strong> Indian plate.1. IntroductionThe Himalayan mountain system has been developing since early Mesozoic time.It is attributed to <strong>the</strong> underthrusting of <strong>the</strong> Indian plate below <strong>the</strong> Eurasian plate.These movements are still continuing and are associated with active seismicity of <strong>the</strong>region where several great earthquakes (Assam 1897 and 1950, Kangra 1905, BiharNepal 1934) have caused huge loss of life and property. Although plate movementshave been taking place for millions of years, a reliable history of great earthquakesin <strong>the</strong> Indian region extends back only 200 years. Of this time period, epicentralparameters of earthquakes based on instrumental data are available for less than acentury.The objective of this paper is to evaluate <strong>the</strong> importance of historical seismicityfor <strong>the</strong> Indian region. This paper describes <strong>the</strong> limitations of earthquake cataloguesfor <strong>the</strong> region. The utility of <strong>the</strong> new catalogue of earthquakes for <strong>the</strong> period 1840 to1900, based on felt reports for peninsular India, and <strong>the</strong> importance of <strong>the</strong> IASPEI<strong>Historical</strong> Seismogram Filming Project are discussed.<strong>Historical</strong> <strong>Seismograms</strong>and Earthquahes of <strong>the</strong> World335Copyright 0 1 Yhb: by .4cademic Press, Inc.All rights of reproduction in any form reserved.

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