The Effects of Double Fault Bends on Rupture Propagation: A Geometrical Parameter Study

被引:103
作者
Lozos, Julian C. [1 ]
Oglesby, David D. [1 ]
Duan, Benchun [2 ]
Wesnousky, Steven G. [3 ]
机构
[1] Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA
[2] Texas A&M Univ, Ctr Tectonophys, Dept Geol & Geophys, College Stn, TX 77843 USA
[3] Univ Nevada, Ctr Neotecton Studies, Reno, NV 89557 USA
关键词
STRIKE-SLIP FAULTS; DYNAMICS; SIMULATIONS; EARTHQUAKES; PRESTRESS; VELOCITY; STRESS; STRAIN;
D O I
10.1785/0120100029
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
We use the 2D finite element method to determine how geometrical parameters determine whether rupture will propagate across a linked stepover in a strike-slip fault. The end segments of the fault system are aligned in the direction of maximum shear, and the length and angle of the linking segment are allowed to vary. We observe that ruptures propagate through extensional stepovers with steeper angles and longer linking segments than otherwise equivalent compressional stepovers. These different rupture behaviors form distinct regions in angle-stepover-length parameter space; the boundary between these regions takes the shape of an asymptotic curve in both the extensional and compressional cases. Models in which the size of the entire fault system was made larger or smaller revealed that the location of the boundaries between regions of different rupture behavior do not scale linearly with the system size; it was easier to rupture steeper and relatively longer stepovers in fault systems that were larger overall. A separate set of models in which the stress field is rotated so that the parallel end segments were optimally aligned for rupture significantly altered the rupture behavior curves; in this stress field, it was easier to rupture compressional stepovers with steeper angles and longer linking segments than it was to rupture equivalent extensional stepovers. In both the case in which the end segments are aligned with the direction of maximum shear and the case in which the end segments are optimally oriented for rupture, the angles at which rupture could no longer propagate through the entire fault corresponded with peaks in the fault's S value.
引用
收藏
页码:385 / 398
页数:14
相关论文
共 23 条
[1]   Fault interactions and large complex earthquakes in the Los Angeles area [J].
Anderson, G ;
Aagaard, B ;
Hudnut, K .
SCIENCE, 2003, 302 (5652) :1946-1949
[2]   RUPTURE PROPAGATION WITH FINITE STRESS IN ANTIPLANE STRAIN [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (20) :3575-3582
[3]   RUPTURE VELOCITY OF PLANE STRAIN SHEAR CRACKS [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (32) :5679-5687
[4]   Effect of normal stress during rupture propagation along nonplanar faults [J].
Aochi, H ;
Madariaga, R ;
Fukuyama, E .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B2)
[5]   Spontaneous rupture propagation on a non-planar fault in 3-D elastic medium [J].
Aochi, H ;
Fukuyama, E ;
Matsu'ura, M .
PURE AND APPLIED GEOPHYSICS, 2000, 157 (11-12) :2003-2027
[6]   NUMERICAL STUDY OF 2-DIMENSIONAL SPONTANEOUS RUPTURE PROPAGATION [J].
DAS, S ;
AKI, K .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1977, 50 (03) :643-668
[7]  
DAY SM, 1982, B SEISMOL SOC AM, V72, P1881
[8]   MODELING OF ROCK FRICTION .1. EXPERIMENTAL RESULTS AND CONSTITUTIVE EQUATIONS [J].
DIETERICH, JH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB5) :2161-2168
[9]   Multicycle dynamics of nonplanar strike-slip faults [J].
Duan, BC ;
Oglesby, DD .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2005, 110 (B3) :1-16
[10]   Heterogeneous fault stresses from previous earthquakes and the effect on dynamics of parallel strike-slip faults [J].
Duan, Benchun ;
Oglesby, David D. .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2006, 111 (B5)