Faulting characteristics of supershear earthquakes

被引:88
作者
Bouchon, Michel [1 ,2 ]
Karabulut, Hayrullah [3 ,4 ]
Bouin, Marie-Paule
Schmittbuhl, Jean [5 ,6 ]
Vallee, Martin [7 ]
Archuleta, Ralph [8 ]
Das, Shamita [9 ]
Renard, Francois [1 ,2 ]
Marsan, David [10 ]
机构
[1] CNRS, Grenoble, France
[2] Univ Grenoble 1, Grenoble, France
[3] Kandilli Observ, Istanbul, Turkey
[4] Earthquake Res Inst, Istanbul, Turkey
[5] CNRS, Strasbourg, France
[6] Univ Strasbourg, Strasbourg, France
[7] Univ Nice, Geosci Azur, Nice, France
[8] Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA
[9] Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England
[10] Univ Savoie, Chambery, France
关键词
Earthquake rupture; Rupture velocity; Fault geometry; Earthquake dynamics; Supershear rupture; 17; AUGUST; 1999; 2001; KOKOXILI-EARTHQUAKE; NORTH ANATOLIAN FAULT; SURFACE RUPTURE; SLIP DISTRIBUTION; IZMIT EARTHQUAKE; DENALI FAULT; TOTSCHUNDA FAULTS; KUNLUN EARTHQUAKE; DUZCE EARTHQUAKE;
D O I
10.1016/j.tecto.2010.06.011
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
Recent observations of large continental strike-slip earthquakes show that different fault segments may rupture at different speeds and that rupture may propagate faster than the shear wave velocity of surrounding rocks. We report that all the documented occurrences of supershear rupture are associated with faults which have simple geometry. The surface trace of these faults is described in the field or seen on satellite images as remarkably linear, continuous and narrow. Segmentation features along these segments are small or absent and the deformation is highly localized. As theoretically predicted, supershear is clearly associated with Mode II rupture. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:244 / 253
页数:10
相关论文
共 63 条
[1]   Near-source ground motions from simulations of sustained intersonic and supersonic fault ruptures [J].
Aagaard, BT ;
Heaton, TH .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2004, 94 (06) :2064-2078
[2]  
akr Z., 2003, Turkish Journal of Earth Sciences, V12, P105
[3]   Surface rupture and slip distribution of the 12 November 1999 Duzce earthquake (M 7.1), North Anatolian fault, Bolu, Turkey [J].
Akyüz, HS ;
Hartleb, R ;
Barka, A ;
Altunel, E ;
Sunal, G ;
Meyer, B ;
Armijo, R .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2002, 92 (01) :61-66
[4]   RUPTURE VELOCITY OF PLANE STRAIN SHEAR CRACKS [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (32) :5679-5687
[5]   The 1999 Izmit, Turkey, earthquake: Nonplanar fault structure, dynamic rupture process, and strong ground motion [J].
Aochi, H ;
Madariaga, R .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2003, 93 (03) :1249-1266
[6]   A FAULTING MODEL FOR THE 1979 IMPERIAL-VALLEY EARTHQUAKE [J].
ARCHULETA, RJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB6) :4559-4585
[7]  
ARPAT E, 2001, 54 GEOL C TURK ABSTR, P7
[8]   Surface ruptures of the 17 August and 12 November 1999 Izmit and Duzce earthquakes in northwestern Anatolia, Turkey: Their tectonic and kinematic significance and the associated damage [J].
Aydin, A ;
Kalafat, D .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2002, 92 (01) :95-106
[9]   The surface rupture and slip distribution of the 17 August 1999 Izmit earthquake (M 7.4), North Anatolian fault [J].
Barka, A ;
Akyüz, HS ;
Altunel, E ;
Sunal, G ;
Çakir, Z ;
Dikbas, A ;
Yerli, B ;
Armijo, R ;
Meyer, B ;
de Chabalier, JB ;
Rockwell, T ;
Dolan, JR ;
Hartleb, R ;
Dawson, T ;
Christofferson, S ;
Tucker, A ;
Fumal, T ;
Langridge, R ;
Stenner, H ;
Lettis, W ;
Bachhuber, J ;
Page, W .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2002, 92 (01) :43-60
[10]   Role of fault branches in earthquake rupture dynamics [J].
Bhat, Harsha S. ;
Olives, Marion ;
Dmowska, Renata ;
Rice, James R. .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2007, 112 (B11)