scholarly journals Coherence of Mach fronts during heterogeneous supershear earthquake rupture propagation: Simulations and comparison with observations

2010 ◽  
Vol 115 (B8) ◽  
Author(s):  
A. Bizzarri ◽  
Eric M. Dunham ◽  
P. Spudich
Keyword(s):  
Earthquake Rupture ◽  
Rupture Propagation

Physics of Earthquake Rupture Propagation

2018 ◽  
Vol 733 ◽  
pp. 1-3
Author(s):  
Shiqing Xu ◽  
Eiichi Fukuyama ◽  
Amir Sagy ◽  
Mai-Linh Doan
Keyword(s):  
Earthquake Rupture ◽  
Rupture Propagation

Spontaneous Complex Earthquake Rupture Propagation

2003 ◽  
Vol 160 (3) ◽  
pp. 579-602 ◽  
Author(s):  
S. Das
Keyword(s):  
Earthquake Rupture ◽  
Rupture Propagation

Models for earthquake rupture propagation

1997 ◽  
Vol 277 (1-3) ◽  
pp. 209-217 ◽  
Author(s):  
J.D. Morgan ◽  
D.L. Turcotte ◽  
J.R. Ockendon
Keyword(s):  
Earthquake Rupture ◽  
Rupture Propagation

Effects of Off-fault Damage on Earthquake Rupture Propagation: Experimental Studies

2009 ◽  
Vol 166 (10-11) ◽  
pp. 1629-1648 ◽  
Author(s):  
Charles G. Sammis ◽  
Ares J. Rosakis ◽  
Harsha S. Bhat
Keyword(s):  
Experimental Studies ◽  
Earthquake Rupture ◽  
Rupture Propagation

scholarly journals Marine forearc structure of eastern Java and its role in the 1994 Java tsunami earthquake

Solid Earth ◽  
2021 ◽  
Vol 12 (11) ◽  
pp. 2467-2477
Author(s):  
Yueyang Xia ◽  
Jacob Geersen ◽  
Dirk Klaeschen ◽  
Bo Ma ◽  
Dietrich Lange ◽  
...  
Keyword(s):  
Seismic Profile ◽  
Earthquake Rupture ◽  
Rupture Propagation ◽  
Slip Model ◽  
Seismic Slip ◽  
Rupture Area ◽  
Seismic Rupture ◽  
Tsunami Earthquake ◽  
Seamount Subduction ◽  
Splay Faults

Abstract. We resolve a previously unrecognized shallow subducting seamount from a re-processed multichannel seismic profile crossing the 1994 Mw 7.8 Java tsunami earthquake rupture area. Seamount subduction occurs where the overriding plate experiences uplift by lateral shortening and vertical thickening. Pronounced back-thrusting at the landward slope of the forearc high and the formation of splay faults branching off the landward flank of the subducting seamount are observed. The location of the seamount in relation to the 1994 earthquake hypocentre and its co-seismic slip model suggests that the seamount acted as a seismic barrier to the up-dip co-seismic rupture propagation of this moderate-size earthquake.

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