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

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

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<strong>Historical</strong> Earthquakes of Thailand, Burma, and Indochina 261101" 104"EI 1KunmingEXPLANATION25'h22Figure 5. Seismic and tectonic structures of Yunnan Province, China and NorthVietnam. Fault information compiled <strong>from</strong> Fontaine and Workman (1978) and TectonicMap of China (1975, in Chinese).3. Magnitude-frequency AnalysisThe seismic data used for this magnitude-frequency analysis is taken <strong>from</strong> variousinternational seismological institutes such as USGS, ISC, and MOS, and <strong>from</strong> <strong>the</strong>Thai Meteorological Department. The area of study is bounded by <strong>the</strong> coordinates5'N to 25'N latitude and 90'E to IlOOE longitude; <strong>the</strong> time period of seismic datais 1900 to 1983.The temporal variation of earthquake occurrence is shown in Figure 8. After<strong>the</strong> year 1960, <strong>the</strong> total number of earthquakes increased due to installation of <strong>the</strong>World-wide Standardized Seismograph Network (WWSSN). The lack of data priorto <strong>the</strong> WWSSN era is due mainly to <strong>the</strong> absence of sufficient seismic instruments.Most of <strong>the</strong> earthquake observations prior to <strong>the</strong> instrumentation era were basedon human perceptions, <strong>the</strong>refore earthquakes having insufficient strength to be feltby an observer would not be recorded.Figure 9 shows <strong>the</strong> magnitude-frequency distribution. The range of magnitudevalue used was mb > 4.0. Figure 9 shows that earthquakes having magnitude 4.5

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