Results 21 to 30 of about 3,038,437 (295)
Long-range, critical-point dynamics in oil field flow rate data [PDF]
, 2006 Earthquake triggering data exhibit long-range spatio-temporal correlations of the power-law form C(l) ∼ l−α and anomalously-slow temporal diffusion of the mean triggering distance of the form: 〈l〉 ∼ tH, with H < 0.5.
Papasouliotis, O. +6 more
core +1 more source
Geophysical Research Letters, 2023 Numerous normal‐faulting aftershocks in subduction forearcs commonly follow large megathrust earthquakes. Postseismic normal faulting has been explained by stress changes induced by the stress drop along the megathrust. However, details of forearc stress
A. Dielforder +5 more
doaj +1 more source
Regional variations in the diffusion of triggered seismicity [PDF]
, 2005 We determine the spatiotemporal characteristics of interearthquake triggering in the International Seismological Centre catalogue on regional and global scales. We pose a null hypothesis of spatially clustered, temporally random seismicity, and determine
Ian G. Main +3 more
core +1 more source
Remote triggering of high magnitude earthquakes along plate boundaries
Scientific Reports, 2022 It has been shown that large magnitude earthquakes can remotely trigger other large magnitude earthquakes within three days. Such triggering of high magnitude earthquakes is potentially indicative of fault systems at the end of their seismic cycles. Here
Robert T. O’Malley +2 more
doaj +1 more source
Multiple fault slip triggered above the 2016 Mw 6.4 MeiNong earthquake in Taiwan
Geophysical Research Letters, 2016 Rapid shortening in convergent mountain belts is often accommodated by slip on faults at multiple levels in upper crust, but no geodetic observation of slip at multiple levels within hours of a moderate earthquake has been shown before.
Mong‐Han Huang +6 more
doaj +1 more source
Earth, Planets and Space, 2020 We propose a normal-stress-dependent Nagata law. Nagata et al. (J Geophys Res 117:B02314, 2012) revised the rate- and state-dependent friction law by introducing the shear stress dependence.
Shingo Yoshida +2 more
doaj +1 more source
Coseismic Stress Change and Viscoelastic Relaxation after the 2008 Great Sichuan Earthquake
Applied Sciences, 2022 Long-term stress accumulation influenced by coseismic stress changes and postseismic viscoelastic relaxation is considered critical to triggering giant earthquakes. Nevertheless, how the stress increase is interrupted by aftershocks and how it influences
Chaodi Xie +6 more
doaj +1 more source
Dizhen xuebao, 2019 为了探究九江—瑞昌地区内的地震活动是否存在动态应力触发关系，本文选用多层黏弹性介质模型，计算了2005年九江—瑞昌MS5.7地震和2011年瑞昌—阳新MS4.6地震产生的动态库仑破裂应力变化。结果显示：九江—瑞昌MS5.7地震产生的动态库仑破裂应力变化，能触发其北东方向的53次地震；瑞昌—阳新MS4.6地震发生后15天内，小震活动增强区及九江—瑞昌MS5.7地震震源区的多次地震活动，可能与其动态应力触发作用有关。
Feifei Dong +6 more
doaj +1 more source
Connection of large earthquakes occurring moment with the movement of the Sun and the Moon and with the Earth crust tectonic stress character [PDF]
Natural Hazards and Earth System Sciences, 2010 It is acceptable that earthquakes certain exogenous (cosmic) triggering factors may exist in every seismoactive (s/a) region and in Caucasus among them. They have to correct earthquake occurring moment or play the triggering role in case when the region ...
M. K. Kachakhidze +4 more
doaj +1 more source
Foreshock migration preceding the 2016 Mw 7.0 Kumamoto earthquake, Japan
Geophysical Research Letters, 2016 We investigated the spatiotemporal evolution of an earthquake sequence following a series of large shallow intraplate earthquakes, including a Mw 6.2 foreshock and Mw 7.0 main shock, in the Kumamoto area of Kyushu, SW Japan.
Aitaro Kato +3 more
doaj +1 more source