Active seismotectonics of the East Anatolian fault
SUMMARY The East Anatolian Fault (EAF) is a 700-km-long left-lateral transform fault
located between the Anatolian and Arabian plates. The proximity of the Euler Pole to the …
located between the Anatolian and Arabian plates. The proximity of the Euler Pole to the …
Sensitivity of Coulomb stress change to the parameters of the Coulomb failure model: A case study using the 2008 Mw 7.9 Wenchuan earthquake
The Coulomb stress change has been widely employed to interpret mainshock‐mainshock
and mainshock‐aftershock triggering as well as interactions amongst earthquake faults and …
and mainshock‐aftershock triggering as well as interactions amongst earthquake faults and …
Crustal velocity images of northwestern Türkiye along the North Anatolian Fault Zone from transdimensional Bayesian ambient seismic noise tomography
SUMMARY Türkiye poses a complex crustal structure and tectonic settings owing to the
northward convergence of the Arabian and African plates with respect to the Anatolian and …
northward convergence of the Arabian and African plates with respect to the Anatolian and …
Coda-derived source properties estimated using local earthquakes in the Sea of Marmara, Türkiye
Accurate estimates of the moment magnitude of earthquakes that physically measure the
earthquake source energy are crucial for improving our understanding of seismic hazard in …
earthquake source energy are crucial for improving our understanding of seismic hazard in …
[PDF][PDF] 2014 年于田犕犛 7.3 地震对后续余震和远场小震活动的动态应力触发
王琼， 解朝娣， 冀战波， 刘建明 - 地球物理学报, 2016 - dsjyj.com.cn
摘要本文采用离散波数法, 计算了2014 年于田犕S7. 3 地震的断层破裂在**场和远场产生的库仑
破裂应力变化, 并结合地震活动特征, 讨论了犕S7. 3 地震对后续余震活动和远场区域小震活动的 …
破裂应力变化, 并结合地震活动特征, 讨论了犕S7. 3 地震对后续余震活动和远场区域小震活动的 …
Statistical and seismotectonic analyses of the Marmara region under existing stress regime in the west of the NAFZ
Abstract The Marmara Region is an active tectonic region in northwestern Türkiye, which
comprises some important strike-slip active fault mechanisms and important tectonic units …
comprises some important strike-slip active fault mechanisms and important tectonic units …
Dynamically triggered aftershock activity and far-field microearthquakes following the 2014 MS7. 3 Yutian, **njiang earthquake
Q WANG, CD XIE, ZB JI, JM LIU - Chinese Journal of Geophysics, 2016 - en.dzkx.org
We systematically examine how dynamic stresses from seismic waves following the 2014
MS7. 3 Yutian, **njiang, earthquake affect aftershocks and regional microseismicity in the …
MS7. 3 Yutian, **njiang, earthquake affect aftershocks and regional microseismicity in the …
[HTML][HTML] Precursory stress changes before large earthquakes; on a new physical law for earthquakes
J Žalohar, B Vičič, M Potočnik, N Soklič… - Journal of Structural …, 2020 - Elsevier
In this article, we first review the progress in our understanding of tectonic stresses in the
Earth's crust achieved in last three to four decades. We briefly review the literature on …
Earth's crust achieved in last three to four decades. We briefly review the literature on …
Synchronization of small-scale seismic clusters reveals large-scale plate deformation
It has long been observed that periods of intense seismic activity in a region alternate with
periods of relative quiescence, but establishing whether or not this intermittency is driven by …
periods of relative quiescence, but establishing whether or not this intermittency is driven by …
The effect of the Wenchuan and Lushan earthquakes on the size distribution of earthquakes along the Longmenshan Fault
Changes in the stress state of faults and their surroundings is a highly plausible mechanism
explaining earthquake interaction. These stress changes can impact the seismicity rate and …
explaining earthquake interaction. These stress changes can impact the seismicity rate and …