Speculations on the geometry of the initiation and termination processes of earthquake rupture and its relation to morphology and geological structure
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[1] The Fracture Energy of Earthquakes , 1975 .
[2] C. Vita-Finzi,et al. Active folding in the Algerian earthquake of 10 October 1980 , 1981, Nature.
[3] G. King,et al. Seismic Potential Revealed by Surface Folding: 1983 Coalinga, California, Earthquake , 1984, Science.
[4] Thomas V. McEvilly,et al. Recurrence models and Parkfield, California, earthquakes , 1984 .
[5] Ralph J. Archuleta,et al. A faulting model for the 1979 Imperial Valley earthquake , 1984 .
[6] R. Sibson. Continental fault structure and the shallow earthquake source , 1983, Journal of the Geological Society.
[7] W. H. Bakun,et al. The Parkfield, California, Prediction Experiment , 1985 .
[8] A. W. Bally,et al. SG 15 Volume 1: Seismic Expression of Structural Styles: A Picture and Work Atlas - Foreword , 1983 .
[9] G. King,et al. Fault related folding near the Wind River thrust, Wyoming, USA , 1983, Nature.
[10] W. H. Bakun,et al. The Parkfield, California, Earthquake Prediction Experiment , 1985, Science.
[11] Models of the complex source of the El Asnam earthquake , 1982 .
[12] D. Boore,et al. Control of rupture by fault geometry during the 1966 parkfield earthquake , 1981 .
[13] G. King,et al. The evolution of a thrust fault system: processes of rupture initiation, propagation and termination in the 1980 El Asnam (Algeria) earthquake , 1984 .
[14] W. Bakun,et al. Earthquakes near Parkfield, California: Comparing the 1934 and 1966 Sequences , 1979, Science.
[15] Ronald L. Bruhn,et al. INTRAPLATE EXTENSIONAL TECTONICS OF THE EASTERN BASIN-RANGE: INFERENCES ON STRUCTURAL STYLE FROM SEISMIC REFLECTION DATA, REGIONAL TECTONICS, AND THERMAL-MECHANICAL MODELS OF BRITTLE-DUCTILE DEFORMATION. , 1984 .
[16] J. Jackson,et al. A seismological study of normal faulting in the Demirci, Alaşehir and Gediz earthquakes of 1969–70 in western Turkey: implications for the nature and geometry of deformation in the continental crust , 1985 .
[17] K. Aki. Characterization of barriers on an earthquake fault , 1979 .
[18] J. Virieux,et al. The evolution of the Gulf of Corinth (Greece): an aftershock study of the 1981 earthquakes , 1985 .
[19] R. Sibson. Stopping of earthquake ruptures at dilational fault jogs , 1985, Nature.
[20] Christopher H. Scholz,et al. Scaling laws for large earthquakes: Consequences for physical models , 1982 .
[21] Keiiti Aki,et al. Fault plane with barriers: A versatile earthquake model , 1977 .
[22] R. Walcott. The kinematics of the plate boundary zone through New Zealand: a comparison of short- and long-term deformations , 1984 .
[23] R. Sibson. Fault zone models, heat flow, and the depth distribution of earthquakes in the continental crust of the United States , 1982 .
[24] C. Vita-Finzi,et al. The seismicity, geomorphology and structural evolution of the Corinth area of Greece , 1985, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.
[25] GEOFFREY KING,et al. Role of Fault Bends in the Initiation and Termination of Earthquake Rupture , 1985, Science.
[26] Geoffrey C. P. King,et al. The accommodation of large strains in the upper lithosphere of the earth and other solids by self-similar fault systems: the geometrical origin of b-Value , 1983 .
[27] Shamita Das,et al. Why large earthquakes do not nucleate at shallow depths , 1983, Nature.