Widespread landslides induced by the Mw 5.1 earthquake of 11 May 2011 in Lorca, SE Spain

被引:67
作者
Alfaro, P. [1 ]
Delgado, J. [1 ]
Garcia-Tortosa, F. J. [2 ]
Lenti, L. [3 ]
Lopez, J. A. [4 ]
Lopez-Casado, C. [5 ]
Martino, S. [6 ]
机构
[1] Univ Alicante, Dpt Ciencias Tierra & Medio Ambiente, E-03080 Alicante, Spain
[2] Univ Jaen, Dpt Dpto Geol, Jaen 23071, Spain
[3] Inst Sci & Technol Transport Dev & Networks, F-75732 Paris 15, France
[4] Inst Ramon Arcas, Lorca 30800, Murcia, Spain
[5] Univ Granada, Dpt Fis Teor & Cosmos, E-18071 Granada, Spain
[6] Univ Roma La Sapienza, Dpt Sci Terra, I-00185 Rome, Italy
关键词
Seismic-induced landslide; Landslide inventory; Shallow earthquake; Moderate magnitude; Topographic site effects; Lorca; STRONG GROUND MOTIONS; DE-MURCIA FAULT; BETIC CORDILLERA; TOPOGRAPHIC AMPLIFICATION; TRAPPED WAVES; ZONE; TECTONICS; ALHAMA; REGION; FAILURES;
D O I
10.1016/j.enggeo.2012.04.002
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
On 11 May 2011, a moderate magnitude (Mw 5.1) earthquake struck the city of Lorca (SE Spain) and nearby areas, causing notable damage, injuries and fatalities. Field inspection of the area affected allowed the location and characterization of more than 250 induced landslides, mainly of disrupted type (rock/soil falls, disrupted soil slides and rock avalanches). This number was very high when compared with the inventories of previous events of similar magnitude (Mw 4.7 to 5.0) in the zone and with the results of previous models for predicting slope behavior during earthquakes. Several factors are proposed here to explain the observed differences: (i) the comparatively high magnitude (Mw 4.5) of a foreshock of the seismic series that may have weakened the slopes; (ii) the high peak ground motion values recorded for these events and (iii) the occurrence of topographic site effects. The results of this study point out the importance of including such effects as improvements in the models for studying the regional behavior of slopes. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:40 / 52
页数:13
相关论文
共 71 条
[1]   Onshore and offshore compressional tectonics in the eastern Betic Cordillera (SE Spain) [J].
Alfaro, P ;
Delgado, J ;
Estévez, A ;
Soria, JM ;
Yébenes, A .
MARINE GEOLOGY, 2002, 186 (3-4) :337-349
[2]  
ARCHULETA RJ, 1982, B SEISMOL SOC AM, V72, P1927
[3]   CLOSURE OF THE AFRICA EURASIA NORTH AMERICA PLATE MOTION CIRCUIT AND TECTONICS OF THE GLORIA FAULT [J].
ARGUS, DF ;
GORDON, RG ;
DEMETS, C ;
STEIN, S .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B5) :5585-5602
[4]  
Ashford SA, 1997, B SEISMOL SOC AM, V87, P692
[5]  
Ashford SA, 1997, B SEISMOL SOC AM, V87, P701
[6]   A shallow fault-zone structure illuminated by trapped waves in the Karadere-Duzce branch of the North Anatolian Fault, western Turkey [J].
Ben-Zion, Y ;
Peng, ZG ;
Okaya, D ;
Seeber, L ;
Armbruster, JG ;
Ozer, N ;
Michael, AJ ;
Baris, S ;
Aktar, M ;
Kuwahara, Y ;
Ito, H .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2003, 152 (03) :699-717
[7]   Earthquake-induced landslides in central America [J].
Bommer, JJ ;
Rodríguez, CE .
ENGINEERING GEOLOGY, 2002, 63 (3-4) :189-220
[8]   Numerical evaluation of slope topography effects on seismic ground motion [J].
Bouckovalas, GD ;
Papadimitriou, AG .
SOIL DYNAMICS AND EARTHQUAKE ENGINEERING, 2005, 25 (7-10) :547-558
[9]   QUATERNARY STRIKE-SLIP FAULTS IN SOUTHEASTERN SPAIN [J].
BOUSQUET, JC .
TECTONOPHYSICS, 1979, 52 (1-4) :277-286
[10]  
BOUSQUET JC, 1974, CR ACAD SCI D NAT, V278, P2617