Abstract
A multi-parametric study of empirical relationships between macroseismic data and magnitude is presented for the Italian region by the analysis of a new extended data set concerning 146 earthquakes. The available magnitude determinations include all of the most intense earthquakes which occurred in Italy in the last century and have been obtained by an accurate revision of original instrumental data. Intensity data have been revised and upgraded on the basis of the most recent studies: only local intensities directly documented have been used. Macroseismic determinations ofM s ,m B andM wa magnitudes have been performed. The empirical relationships between maximum felt intensity (I max ) and magnitude have been determined by the use of a distribution-free approach and a linear regression analysis. This last parameterization allows for the explanation of more than 60% of the variation in magnitude. In order to improve these results, the linear dependence between magnitude,I max and average distances (in logarithm) corresponding to fixed attenuation values has been explored. The comparison between instrumental magnitudes and corresponding macroseismic estimates obtained from empirical relationships shows that the respective uncertainties are comparable.
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References
Albarello, D., Mucciarelli, M., andMantovani, E. (1990),Empirical Magnitude-intensity Relationships: A Non-parametric Approach, Proc. XXI ESC General Assembly, Barcelona, Spain, 871–874.
Ambraseys, N. N. (1985),Magnitude assessment of Northwestern European Earthquakes, Earthq. Eng. Struct. Dyn.13, 307–320.
Ambraseys, N. N. (1988),Engineering Seismology, Earthq. Eng. Struct. Dyn.17 (1), 1–106.
Ambraseys, N. N., andMelville, C. P.,A History of Persian Earthquakes, Cambridge Earth Sciences Series (Cambridge University Press, Cambridge, (1982), 219 pp.
Basili, A., Marcelli, L., andSmriglio, G. (1980),La magnitudo macrosismica come funzione di Io e h, Annali di Geofisica33, 37–66.
Båth, M. (1981),Earthquake Magnitude—Recent Research and Current Trends, Earth Sci. Rev.17, 315–398.
Benouar, D. (1994),The Seismicity of Algeria and Adjacent Regions, Ann. Geofis.,XXXVII (4), 459–557.
Berardi, R., Magri, L., andMucciarelli, M. (1990),Do Different Experts and Computer Programs Agree on the Interpretation of the Same Intensity Map? Proc. XXII ESC General Assembly, Barcelona, Spain, 371–376.
Caputo, M. (1983),Are There One-to-one Relationships Between Magnitude, Moment, Intensity and Ground Acceleration? Geophys. J. R. Astr. Soc.72, 83–92.
Di Maro, R., andTertulliani, A. (1990),The Relation between Intensity and Magnitude for Italian Earthquakes, Pure Appl. Geophys.132, 711–718.
Draper, N. R., andSmith, H. Applied Regression Analysis (Wiley, New York 1966), 407 pp.
Durbin, J., andWatson, G. S. (1951),Testing for Serial Correlation in Least Squares Regression, Biometrika38, 159–178.
Galanopoulos, A. G. (1961),On Magnitude Determination Using Macroseismic Data, Annali di GeofisicaXIV (3), 225–253.
Gutenberg, P. (1945),Amplitudes of Surface Waves and Magnitude of Shallow Earthquakes, Bull. Seismol. Soc. Am.35, 57–69.
Gutenberg, B. andRichter, C. F. (1956),Earthquake Magnitude, Intensity, Energy and Acceleration (second paper), Bull. Seismol. Soc. Am.46.
Kanamori, H. (1978),Quantification of Earthquakes, Nature271 411–414.
Karnik, V.,The Seismicity of the European Area (Reidel Publ. Co., Dordrecht 1969), 364 pp.
Karnik, V., Kondorskaya, N. V., Riznichenco, Y. V., Savarensky, Y. F., Solovev, S. L., Shebalin, N. V., Vanek, J., andZatopek, A. (1962)Standardization of Earthquake Magnitude Scales, Studia Geophys. et Geoet.6, 41–48.
Kendall, M.-G. (1938),A New Measure of Rank Correlation, Biometrika30, 81–93.
Kendall, M. G.,Rank Correlation Methods (Griffin Co., London 1955), 195 pp.
Margottini, C., Ambraseys, N., andScrepanti, A. (1993a),La magnitudo dei terremoti Italiani del XX secolo, ENEA Monography, Rome, 57 pp.
Margottini, C., Martini, G., andSlejko, D. (1993b),Instrumental Seismological Data since 1900 for North Eastern Italy, Earthq. Eng. Struct. Dyn.22, 1017–1030.
Paciello, A. (1988),Some aspects of the hazard analysis for an Italian region. InHistorical Seismicity in Central Eastern Mediterranean region (Serva, L., and Margottini, C., eds.), (ENEA-IAEA 1988) pp. 245–258.
Peronaci, M. (1982),Intensity-magnitude Relationships for Italian Regions, Boll. Geofis. Teor. Appl.XXIV (94), 121–128.
Postpischl, D., ed. (1984),Catalogo dei terremoti italiani dall'anno 1000 al 1980, Quaderni della Ricerca Scientifica114 (2B), 164 pp.
Richter, C. F. (1935),An Instrumental Earthquake Magnitude Scale, BSSA25, 1–32.
Rock, N. M. S. (1988),Numerical Geology, Lecture Notes in Geosciences Springer Verlag, Berlin, 427 pp.
Sibol, M. S., Bollinger, P. A., andBirch, J. B. (1987)Estimation of Magnitudes in Central and Eastern North America Using Intensity and Felt Area, Bull. Seismol. Soc. Am.77, (5), 1635–1654.
Tinti, S., Vittori, T., andMulargia, F. (1986),Regional Intensity-magnitude Relationships for the Italian Territory, Tectonophys.127, 129–154.
Zatopek, A., andChristoskov, L. (1969),On the True Value of A/T for the First Maximum of Dumped Harmonic Ground Movement for Directly Recording Pendulums, Bull. Int. Inst. Seismol. Earth. Eng.6, 63–80.
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Albarello, D., Berardi, A., Margottini, C. et al. Macroseismic estimates of magnitude in Italy. PAGEOPH 145, 297–312 (1995). https://doi.org/10.1007/BF00880272
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DOI: https://doi.org/10.1007/BF00880272