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

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320 De-yi Feng, “ding-zhou Lin, and Kun-yuan ZhuangFor pz, p3, and p4, <strong>the</strong> upward semi-normal distribution niny be taken as: p(z) =0, or p(z) = 1 - exp[-k(z - a)’]. On <strong>the</strong> basis of empirical data, we have obtained<strong>the</strong> following preliniiiinry results:p2 = 0 for 0 5 z 5 0.3, or p2 = 1 - exp[-69.S1(z - 0.S)2] for 0.3 < z.p3 = 1 - exp[-0.011~’].p4 = 0 for 0 5 z 5 50, or p4 = 1 - exp[-O.OOl(z - for 50 < z.For ps, <strong>the</strong> downward semi-normal distribution is taken as p(z) = exp[-kz’].When 5 = 30°, we took p = 0.5, so that k = 2.5. Then we have pug = exp[-2.5~~1.The parameter z in <strong>the</strong> expressions of p2, p3, p4, and p5 is in units of kilometers,meters, kilometers, and radians, respectively.(2) Landslide. We can take tlie downward semi-normal distribution as p(z) =exp[-kz’], where z is <strong>the</strong> slope angle measured in radians, k is an empirical coefficientdepending on earthiness and saturation. For non-saturated loessial mild clay,k = 3.61.4.2. Example of ApplicationAn example was taken <strong>from</strong> tlie Seismological Bureau of Shanxi (1982). At <strong>the</strong>old Yulin grike of Kangding 011 <strong>the</strong> Xiansliuihe fault zone, where <strong>the</strong> slope angle is28”, <strong>the</strong> accuniulation of many collapsed bodies was discovered.Based on tlie thkd criterion, <strong>from</strong> p3 = exp[-2.5z2], we obtain p3 = 0.547 > 0.5.As mentioned above, this phenomenon may be recognized as a possible relic ofpale oe art 11 quake.5. DiscussionsIt should be emphasized that this paper is mainly for describing methods of fuzzyresearch. It is only a first step that we have done. Obviously, <strong>the</strong> methods suggestedby <strong>the</strong> authors need to be fur<strong>the</strong>r exaniined, tested and developed in <strong>the</strong> future.REFERENCESDubois, D. and H. Prade (1980). Fuzzy Sets and Systems: Theory and Application, AcademicPress.Feng, D. Y. and X. H. Liu (Editors) (1985). Fuzzy Ma<strong>the</strong>matics in Earthquake Research,Seismological Press of China.Feng, D. Y., M. Z. Lin, and o<strong>the</strong>rs (1983~). Application of fuzzy integrated evaluationarid close press to <strong>the</strong> studies of seismic source, Di Zhen (Earthquake), No. 4.Feng, D. Y., S. B. LOU, and o<strong>the</strong>rs (1983b). The Methods of Fuzzy Ma<strong>the</strong>matics and TheirApplicatzons, Seismological Press of China.Feng, D. Y., S. B. Lou, and o<strong>the</strong>rs (1934). Quantitative evaluation of earthquake intensitybased on <strong>the</strong> fuzzy standards of seismic scale, Proceedings of Eighth World Conferenceon Earthquake Engineering, Vol. 11, 819-828, San Francisco.Gu, G. X. (Editor) (1983). Catalogue of Earthquakes in China, Scientific Press.Seismological Bureau of Sansi (1982), Papers of Prehistoric Earthquakes and QuaternaryGeology, Scientific Technical Press of Sansi.Seismological Institute of Lanzhou and Seismological Bureau of Ningxia (1980). The 1920Haiyuan Great Earthquake, Seismological Press of China.

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