The major asperities of the 1999 Mw = 7.4 Izmit earthquake defined by the microseismicity of the two decades before it
暂无分享,去创建一个
[1] N. N. Ambraseys,et al. Long‐term seismicity of Istanbul and of the Marmara Sea region , 1991 .
[3] H. Kahle,et al. Active crustal deformation in the Marmara Sea Region, NW Anatolia, Inferred from GPS measurements , 1995 .
[4] Stefan Wiemer,et al. Mapping the B‐value anomaly at 100 km depth in the Alaska and New Zealand Subduction Zones , 1996 .
[5] M. Wyss,et al. Mapping asperities by minima of local recurrence time: San Jacinto‐Elsinore fault zones , 2000 .
[6] M. Wyss,et al. The Alaska earthquake of 28 March 1964: A complex multiple rupture , 1967 .
[7] C. Frohlich,et al. Teleseismic b values; Or, much ado about 1.0 , 1993 .
[8] Keiiti Aki,et al. Asperities, barriers, characteristic earthquakes and strong motion prediction , 1984 .
[9] P. Reasenberg. Second‐order moment of central California seismicity, 1969–1982 , 1985 .
[10] Y. Ogata,et al. Analysis of temporal and spatial heterogeneity of magnitude frequency distribution inferred from earthquake catalogues , 1993 .
[11] Ian G. Main,et al. Temporal variations of the fractal properties of seismicity in the western part of the north Anatolian fault zone: possible artifacts due to improvements in station coverage , 1995 .
[12] I. Main,et al. Temporal variations in the fractal properties of seismicity in the North Anatolian Fault Zone between 31°E and 41°E , 1996 .
[13] F. Amelung,et al. Earthquake scaling laws for creeping and non‐creeping faults , 1997 .
[14] Bertrand Meyer,et al. Westward propagation of the North Anatolian fault into the northern Aegean: Timing and kinematics , 1999 .
[15] Stefan Wiemer,et al. Two current seismic quiescences within 40 km of Tokyo , 1997 .
[16] G. Latham,et al. An experimental study of thermally induced microfracturing and its relation to volcanic seismicity , 1970 .
[17] R. Young,et al. Space-time correlations ofb values with stress release , 1992 .
[18] M. N. Toksöz,et al. Space-time migration of earthquakes along the North Anatolian fault zone and seismic gaps , 1979 .
[19] C. Scholz. The frequency-magnitude relation of microfracturing in rock and its relation to earthquakes , 1968 .
[20] Stefan Wiemer,et al. Variations in the frequency‐magnitude distribution with depth in two volcanic areas: Mount St. Helens, Washington, and Mt. Spurr, Alaska , 1997 .
[21] Ömer Alptekin,et al. Effect of Aftershocks on Earthquake Hazard Estimation: An Example from the North Anatolian Fault Zone , 1999 .
[22] I. Main,et al. Spatial variations of the fractal properties of seismicity in the Anatolian fault zones , 1996 .
[23] T. Wilson,et al. Size scaling relationships in the active fault networks of Japan and their correlation with Gutenberg‐Richter b values , 2001 .
[24] S. Crampin,et al. The Seismicity of the Marmara Sea Region of Turkey , 1975 .
[25] G. King,et al. Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea , 1996 .
[26] H. Kanamori,et al. The asperity model and the nature of large subduction zone earthquakes. , 1982 .
[27] N. N. Ambraseys,et al. Some characteristic features of the Anatolian fault zone , 1970 .
[28] Yan Y. Kagan,et al. Long-term earthquake clustering , 1991 .
[29] M. Wyss. Towards a Physical Understanding of the Earthquake Frequency Distribution , 1973 .
[30] Reporting history of the Central Aleutians Seismograph Network and the quiescence preceding the 1986 Andreanof Island earthquake , 1991, Bulletin of the Seismological Society of America.
[31] M. Wyss,et al. Most- and Least-Likely Locations of Large to Great Earthquakes along the Pacific Coast of Mexico Estimated from Local Recurrence Times Based on b-Values , 2001 .
[32] M. Wyss,et al. Mapping the frequency-magnitude distribution in asperities: An improved technique to calculate recurrence times? , 1997 .