Long-term seismic regime reconstruction using paleoseismological data

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• 作者：E. Rogozhin (1)
  
  1. Institute of Physics of the Earth ; Russian Academy of Sciences ; 10 ; B. Gruzinskaya st. ; Moscow ; 123995 ; Russia
  
• 关键词：Magnitude ; Earthquake ; Intensity ; Rupture ; Seismic fault ; Liquefaction ; Active fault ; Paleoseismology
• 刊名：Acta Geodaetica et Geophysica
• 出版年：2015
• 出版时间：March 2015
• 年：2015
• 卷：50
• 期：1
• 页码：63-77
• 全文大小：3,943 KB
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  10. Rogozhin, EA Reconstruction of long-term seismic regime using paleoseismogeological data. In: Laverov, NP eds. (2010) Extreme natural phenomena and catastrophes. V. 1: evaluation and ways to reduce the negative effects of extreme weather events. IPE RAS, Moscow, pp. 44-64
  11. Rogozhin, EA, Jun, Shen, Rodina, SN (2013) Comparison of seismotectonic peculiarities of Altai Mountains and Mongolian Altai. Seism Instrum 49: pp. 285-296 CrossRef
  12. Rogozhin, EA, Novikov, PP, Rodina, SN (2010) Paleoseismic ruptures and the long-term seismic regime of the Koryak uplands. Geophys Stud 11: pp. 35-43
  13. Rogozhin, EA, Ovsyuchenko, AN, Marahanov, AV (2008) Strongest earthquakes in the south of the Mountain Altai in the Holocene. Phys Solid Earth 44: pp. 469-486 CrossRef
  14. Rogozhin EA, Ovsyuchenko AN, Marakhanov AV, Novikov SS (2009) Tectonic position and geological manifestations of the 2006 Olyutor earthquake in Koryakiya. Geotectonics (6):3鈥?3. doi:10.1134/S0016852109060016
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• 刊物主题：Geophysics/Geodesy;
• 出版者：Springer Netherlands
• ISSN：2213-5820

文摘

Series of geologically and seismically active ruptures with amplitudes of vertical and horizontal dislocations from some tens of centimeters up to 2.5 m was studied using the paleoseismological method within mobile folded systems of Northern Eurasia (the Mountain Altai and the north of the Kamchatka region) during the field works for the last decade. The paleoseismological materials have been used to estimate the seismic regime of the specified regions for the major Holocene. Micro- and macroseismic data of strong seismic events of these regions were also used, including the latest strong seismic shocks of 2003 and 2006. The results demonstrate rectilinear recurrence diagrams throughout the whole range of magnitudes in the two regions of Northern Eurasia explored. It means that the seismic regime at the Late Quaternary of the geological history has remained almost unchanged.