نتایج جستجو برای: fault earthquake

تعداد نتایج: 90662  

2013
Subrata Kr. Debnath

The process of stress accumulation near earthquake faults during the aseismic period in between two major seismic events in seismically active regions has become a subject of research during the last few decades. Earthquake fault of finite length of strike-slip nature in a viscoelastic layer over a viscoelastic half space representing the lithosphere-asthenosphere system has been considered her...

2018
Gregory C. Beroza Takeshi Mikumo

Recent studies of strong motion data consistently show that the risetime (duration of slip at particular locations on the fault) is significantly shorter than the overall rupture duration. The physical explanation for this observation and its implications have become central issues in earthquake source studies. Two classes of mechanisms have been proposed to explain short risetimes. One explana...

2005
Thomas H. Heaton

We have determined a source rupture model for the 1992 Landers earthquake (Mw 7.2) compatible with multiple data sets, spanning a frequency range from zero to 0.5 Hz. Geodetic survey displacements, near-field and regional strong motions, broadband teleseismic waveforms, and surface offset measurements have been used explicitly to constrain both the spatial and temporal slip variations along the...

2003
Chen Ji Donald V. Helmberger David J. Wald Kuo-Fong Ma

[1] We investigate the rupture process of the 1999 Chi-Chi, Taiwan, earthquake using extensive near-source observations, including three-component velocity waveforms at 36 strong motion stations and 119 GPS measurements. A three-plane fault geometry derived from our previous inversion using only static data [Ji et al., 2001] is applied. The slip amplitude, rake angle, rupture initiation time, a...

2017
Tianhaozhe Sun Kelin Wang Toshiya Fujiwara Shuichi Kodaira Jiangheng He

During the 2011 magnitude 9 Tohoku-oki earthquake, very large slip occurred on the shallowest part of the subduction megathrust. Quantitative information on the shallow slip is of critical importance to distinguishing between different rupture mechanics and understanding the generation of the ensuing devastating tsunami. However, the magnitude and distribution of the shallow slip are essentiall...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 1996
J H Dieterich B Kilgore

The rate- and state-dependent constitutive formulation for fault slip characterizes an exceptional variety of materials over a wide range of sliding conditions. This formulation provides a unified representation of diverse sliding phenomena including slip weakening over a characteristic sliding distance Dc, apparent fracture energy at a rupture front, time-dependent healing after rapid slip, an...

Journal: :Science 2017
Andre Hüpers Marta E Torres Satoko Owari Lisa C McNeill Brandon Dugan Timothy J Henstock Kitty L Milliken Katerina E Petronotis Jan Backman Sylvain Bourlange Farid Chemale Wenhuang Chen Tobias A Colson Marina C G Frederik Gilles Guèrin Mari Hamahashi Brian M House Tamara N Jeppson Sarah Kachovich Abby R Kenigsberg Mebae Kuranaga Steffen Kutterolf Freya L Mitchison Hideki Mukoyoshi Nisha Nair Kevin T Pickering Hugo F A Pouderoux Yehua Shan Insun Song Paola Vannucchi Peter J Vrolijk Tao Yang Xixi Zhao

Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected, increasing earthquake and tsunami size. International Ocean Discovery Program Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within the deep sediments. Thermal modeling links this freshening to amorphous sil...

2017
Matt J Ikari Achim J Kopf

The near-surface areas of major faults commonly contain weak, phyllosilicate minerals, which, based on laboratory friction measurements, are assumed to creep stably. However, it is now known that shallow faults can experience tens of meters of earthquake slip and also host slow and transient slip events. Laboratory experiments are generally performed at least two orders of magnitude faster than...

2006
Rémi Michel Jean-Philippe Avouac

[1] Coseismic deformation of the ground can be measured from aerial views taken before and after an earthquake. We chose the area of the Kickapoo-Landers step over along the 1992 Landers earthquake zone, using air photos (scale 1:40,000) scanned at 0.4 m resolution. Two photos acquired after the earthquake are used to assess the accuracy and to evaluate various sources of noise. Optical distort...

2017
Hideo Aochi Thomas Ulrich

We perform numerical simulations of dynamic rupture processes along the North Anatolian fault in the Sea of Marmara, which poses a high risk to the nearby city of Istanbul. Several fault geometry models, nucleation points, and initial stress states are tested. The likelihood of each earthquake scenario is evaluated, and a probabilistic assessment of the ground-motion estimation is proposed. The...

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