Coulomb interactions and the 17 August 1999 Izmit, Turkey earthquake

[1]  R. Armijo,et al.  Morphology, displacement, and slip rates along the North Anatolian Fault, Turkey , 2002 .

[2]  Bertrand Meyer,et al.  Surface Rupture and Slip Distribution of the 12 November 1999 Düzce Earthquake (M 7.1), North Anatolian Fault, Bolu, Turkey , 2002 .

[3]  N. Ambraseys The earthquake of 10 July 1894 in the Gulf of Izmit (Turkey) and its relation to the earthquake of 17 August 1999 , 2001 .

[4]  Massimo Cocco,et al.  Fault interaction by elastic stress changes: New clues from earthquake sequences , 2001 .

[5]  A. Barka,et al.  Heightened odds of large earthquakes near istanbul: An interaction-based probability calculation , 2000, Science.

[6]  Demitris Paradissis,et al.  Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus , 2000 .

[7]  R. Armijo,et al.  The fault breaks of the 1999 earthquakes in Turkey and the tectonic evolution of the Sea of Marmara; a summary , 2000 .

[8]  A. Barka,et al.  The 1999 İzmit and Düzce earthquakes : preliminary results , 2000 .

[9]  A. Barka,et al.  The 17 August 1999 Izmit Earthquake , 1999, Science.

[10]  Bertrand Meyer,et al.  Westward propagation of the North Anatolian fault into the northern Aegean: Timing and kinematics , 1999 .

[11]  J. Dieterich,et al.  Stress transferred by the 1995 Mw = 6.9 Kobe, Japan, shock: Effect on aftershocks and future earthquake probabilities , 1998 .

[12]  Masson,et al.  Tomographic evidence for localized lithospheric shear along the altyn tagh fault , 1998, Science.

[13]  James Jackson,et al.  Faulting associated with historical and recent earthquakes in the Eastern Mediterranean region , 1998 .

[14]  Aurélia Hubert-Ferrari La faille nord-anatolienne (cinematique, morphologie, localisation, vitesse et decalage total) et modelisations utilisant la contrainte de coulomb sur differentes echelles de temps , 1998 .

[15]  H. Kahle,et al.  GPS and geologic estimates of the tectonic activity in the Marmara Sea region, NW Anatolia , 1997 .

[16]  W. H. Bakun,et al.  Estimating earthquake location and magnitude from seismic intensity data , 1997, Bulletin of the Seismological Society of America.

[17]  P. Adler,et al.  Fluid flow triggered migration of events in the 1989 Dobi Earthquake sequence of central Afar , 1997 .

[18]  Robert W. King,et al.  Global Positioning System measurements of present‐day crustal movements in the Arabia‐Africa‐Eurasia plate collision zone , 1997 .

[19]  James H. Dieterich,et al.  Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering , 1997 .

[20]  G. King,et al.  Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea , 1996 .

[21]  G. King,et al.  STATIC STRESS CHANGES AND THE TRIGGERING OF EARTHQUAKES , 1994 .

[22]  J. Dieterich A constitutive law for rate of earthquake production and its application to earthquake clustering , 1994 .

[23]  Y. Okada Internal deformation due to shear and tensile faults in a half-space , 1992, Bulletin of the Seismological Society of America.

[24]  N. N. Ambraseys,et al.  Long‐term seismicity of Istanbul and of the Marmara Sea region , 1991 .

[25]  A. Barka,et al.  Strike‐slip fault geometry in Turkey and its influence on earthquake activity , 1988 .

[26]  D. L. Anderson,et al.  Theoretical Basis of Some Empirical Relations in Seismology by Hiroo Kanamori And , 1975 .

[27]  N. N. Ambraseys,et al.  Some characteristic features of the Anatolian fault zone , 1970 .