Integrated transnational macroseismic data set for the strongest earthquakes of Vrancea (Romania)

被引:40
|
作者
Kronrod, Tatiana [1 ]
Radulian, Mircea [2 ]
Panza, Giuliano [3 ,4 ]
Popa, Mihaela [2 ]
Paskaleva, Ivanka [5 ]
Radovanovich, Slavica [6 ]
Gribovszki, Katalin [7 ]
Sandu, Ilie [8 ]
Pekevski, Lazo [9 ]
机构
[1] Int Inst Earthquake Predict Theory & Math Geophys, Moscow 117997, Russia
[2] Natl Inst Earth Phys, Bucharest 76900, Romania
[3] Univ Trieste, Dipartimento Matemat & Geosci, I-34127 Trieste, Italy
[4] Abdus Salam Int Ctr Theoret Phys, I-34014 Trieste, Italy
[5] BAS, CLSMEE, Sofia 1113, Bulgaria
[6] Seismol Survey Serbia, Belgrade 11216, Serbia
[7] Hungarian Acad Sci, Geodet & Geophys Res Inst, H-9400 Sopron, Hungary
[8] Moldavian Acad Sci, Inst Geol & Seismol, Kishinev, Moldova
[9] Seismol Observ, Skopje 1000, Macedonia
关键词
Vrancea; Intermediate-depth earthquake; Macroseismic data and fields; Isoseismals; Diffused boundary method; SEISMIC HAZARD; MARCH; 4; WAVE ATTENUATION; ISOSEISMAL MAP; INVERSION; BENEATH; REGION; INTENSITIES; TOMOGRAPHY; TENSOR;
D O I
10.1016/j.tecto.2013.01.019
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A unique macroseismic data set for the strongest earthquakes occurring since 1940 in the Vrancea region is constructed by a thorough review of all available sources. Inconsistencies and errors in the reported data and in their use are also analysed. The final data set, which is free from inconsistencies, including those at the political borders, contains 9822 observations for the strong intermediate-depth earthquakes: 1940, M-w = 7.7; 1977, M-w = 7.4; 1986, M-w = 7.1; 1990, May 30, M-w = 6.9; 1990, May 31, M-w = 6.4; and 2004, M-w = 6.0. This data set is available electronically as Supplementary data to the present paper. From the discrete macroseismic data, the continuous macroseismic field is generated using the methodology developed by Molchan et al. (2002). The procedure, along with the unconventional (smoothing method) modified polynomial filtering (MPF), uses the diffuse boundary (DB) method, which visualises the uncertainty in the isoseismal boundaries. The comparison of DBs with previous isoseismal maps supplies a good evaluation criterion of the reliability of earlier published maps. The produced isoseismals can be used not only for the formal comparison of the observed and theoretical isoseismals, but also for the retrieval of source properties and the assessment of local responses (Molchan et al., 2011). (c) 2013 Elsevier B.V. All rights reserved.
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页码:1 / 23
页数:23
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