Results 261 to 270 of about 71,778 (287)
Some of the next articles are maybe not open access.
Coulomb stress changes at calderas: Modeling the seismicity of Campi Flegrei (southern Italy)
Journal of Geophysical Research: Solid Earth, 2003The local seismicity occurring at Campi Flegrei caldera during a recent unrest (1982–1984) has been modeled in terms of Coulomb stress changes due to magma chamber overpressure, superimposed on a background tensile regional stress. The computations, performed by a finite element method in heterogeneous axial‐symmetric elastic models, also take into ...
Claudia Troise +2 more
openaire +1 more source
Coulomb Stress Changes after 11 May 2017 Askale-Erzurum(NETurkey) Earthquake (Mw = 4.7)
2020Erzurum city NE Turkey , one of the largest provinces of the eastern Anatolia region are surrounded by many active tectonic units. These tectonic units generated many earthquakes that led to the loss of life and property during the historical and instrumental period.
OZER, Caglar, BAYRAK, Erdem
openaire +2 more sources
2022
<p>Sufficient shreds of evidence have proved the existence of the remote triggering effect of large earthquakes. To understand its mechanism, it is necessary to conduct detailed investigations on the influence of the far-field dynamic stress changes on the stress state of faults.
Fuzhen Li +4 more
openaire +1 more source
<p>Sufficient shreds of evidence have proved the existence of the remote triggering effect of large earthquakes. To understand its mechanism, it is necessary to conduct detailed investigations on the influence of the far-field dynamic stress changes on the stress state of faults.
Fuzhen Li +4 more
openaire +1 more source
Coulomb stress changes due to main earthquakes in Southeast Iran during 1981 to 2011
Journal of Seismology, 2018Southeast of Iran experienced eight destructive earthquakes during 30 years from 1981 to 2011. Six of these events with M > 6.5 were fatal and caused great human and financial losses in the region. The 1981 July 28 (Mw 7.2) Sirch earthquake with 65 km surface rupture was the largest event in this region since 1877 and with other three earthquakes ...
Behnam Maleki Asayesh +2 more
openaire +1 more source
Modelling of Coulomb stress changes during the great (Mw = 8.8) 1906 Colombia-Ecuador earthquake
Journal of South American Earth Sciences, 2016Abstract Six alternative models of slip distribution during the 1906 Esmeraldas (Mw = 8.8) megathrust earthquake are used to compute Coulomb stress changes on two types of specific faults and onto optimal strike-slipe faults along the Colombia-Ecuador Pacific region.
Edwin F. Mayorga, John J. Sánchez
openaire +1 more source
COULOMB STRESS CHANGES FROM GROUPED MAGNITUDE 7+ EARTHQUAKES IN SOUTH ITALY
2006http://www.ism.ac.jp/~ogata/Statsei4/programme ...
NERI, Giancarlo +2 more
openaire +1 more source
Coulomb stress change due to 2005 Kashmir earthquake and implications for future seismic hazards
Journal of Seismology, 2008We calculate static stress change due to the 2005 Kashmir earthquake (M = 7.6). We suggest that the earthquake caused significant increase in stress in the Indo-Kohistan seismic zone (IKSZ) region, lying to the NW of the rupture and moderate increase in the adjacent Himalayan region, lying to the SE of rupture.
openaire +1 more source
Coulomb stress models for the 2019 Ridgecrest, California earthquake sequence
Tectonophysics, 2020Walter D Mooney
exaly