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

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3 44 H. N. Snvastava and S. K. Das5. IASPEI <strong>Historical</strong> Seismogram Filming Project<strong>Seismograms</strong> of earthquakes recorded on photographic paper have a tendency todeteriorate with time under changing wea<strong>the</strong>r conditions. They require a large storageplace, greater care in handling, and special precautions to prevent damage <strong>from</strong>white ants. Due to <strong>the</strong> rapid developments in modern seismological instrumentationof digital as well as analog type, a tendency has been noticed among some seismologiststo undermine <strong>the</strong> utility of old records which were obtained through low-gaininstruments like Omori-Ewing, Wiechert, Milne-Shaw, and Wood- Anderson. Therecent development of new techniques of digitization and modern methods of analysishave increased <strong>the</strong> utility of old records to supplement results pertaining tosource mechanism studies, crustal and upper mantle structure, etc. The IASPEI<strong>Historical</strong> Seismogram Filming Project will ensure <strong>the</strong> preservation and availabilityof old seismic records for a long time in <strong>the</strong> future. Among <strong>the</strong> Indian seismologicalstations, Bombay has been selected as one of <strong>the</strong> stations for participation in <strong>the</strong><strong>Historical</strong> Seismogram Filming Project, and more than 20,000 seismograms havebeen microfilmed so far.Table 1 lists <strong>the</strong> instruments and <strong>the</strong> seismological stations that were in operationduring 1962. Because of storage of some seismograms at damp places like Calcuttaand Bombay, some records have been lost due to white ants.During <strong>the</strong> last few years, <strong>the</strong>re has been a rapid advancement in understanding<strong>the</strong> nature of stress and source parameters of earthquakes in India and elsewhere(Ichikawa et al., 1972; Tandon and Srivastava, 1975; Srivastava and Chaudhury,1979; and many o<strong>the</strong>rs). The <strong>Historical</strong> Seismogram Filming Project will enableseismologists to study <strong>the</strong>se aspects in detail <strong>from</strong> near as well as far field anglebased on similar records in Europe, India, Japan, and many o<strong>the</strong>r countries.6. Significant Seismological Problems in <strong>the</strong> Indian RegionThe following seismological problems are of immediate interest for <strong>the</strong> Indianregion for which <strong>the</strong> <strong>Historical</strong> Seismogram Filming Project may provide additionaldata:(I) The catalogue of earthquakes (Tandon and Srivastava, 1974) gives a range ofmagnitudes for many earthquakes in <strong>the</strong> Indian region. Refinement of methodsof magnitude determination <strong>from</strong> historical seismograms will enable us to assign amore realistic value in different Indian regions <strong>from</strong> <strong>the</strong> point of view of risk analysis.(2) A number of reliable fault-plane solutions of earthquakes in and around <strong>the</strong>Indian plate (Ichikawa et al., 1972; Tandon and Srivastava, 1975) suggest refinementof regional plate tectonics models. A few studies have been made for someearthquakes in <strong>the</strong> Indian region prior to 1962 using body waves (Ichikawa et al.,1972, and o<strong>the</strong>rs). However, <strong>the</strong>re is a need for detailed studies to evaluate stressdrop, seismic moment and related parameters which may enable us to explain <strong>the</strong>difference of energy released between earthquakes near plate boundaries and within<strong>the</strong> plate, prior to 1962.

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