Results 101 to 110 of about 7,164 (223)

Dynamic Earthquake Source Inversion With Generative Adversarial Network Priors

Journal of Geophysical Research: Solid Earth, Volume 131, Issue 3, March 2026.
Abstract Dynamic earthquake source inversion consists of inferring frictional parameters and initial stress on a fault consistent with recorded seismological and geodetic data and with dynamic earthquake rupture models. In a Bayesian inversion approach, the nonlinear relationship between model parameters and data requires a computationally demanding ...
Jan Premus, Jean Paul Ampuero
wiley   +1 more source

Geodetic displacements and aftershocks following the 2001 M_w = 8.4 Peru earthquake: Implications for the mechanics of the earthquake cycle along subduction zones [PDF]

, 2005
We analyzed aftershocks and postseismic deformation recorded by the continuous GPS station AREQ following the M_w = 8.4, 23 June 2001 Peru earthquake. This station moved by 50 cm trenchward, in a N235°E direction during the coseismic phase, and continued
Avouac, J.-P., Perfettini, H., Ruegg, J.-C.   +2 more
core   +3 more sources

High‐Precision Aftershock Distribution Highlights the Complex Fault Geometry of the 2024 Mw 7.5 Noto Peninsula Earthquake

Geophysical Research Letters, Volume 53, Issue 4, 28 February 2026.
Abstract We deployed 30 temporary seismic stations around the source region of the 2024 Mw 7.5 Noto Peninsula earthquake to investigate the relationship between mainshock rupture and fault geometry. Using machine learning techniques, we detected and precisely located 46,252 aftershocks, revealing several fault planes corresponding to active faults ...
Hidenobu Takahashi, Yasuhira Aoyagi, Keisuke Yoshida, Haruo Kimura, Eiji Kurashimo, Shinichi Sakai   +5 more
wiley   +1 more source

Coseismic horizontal slip revealed by sheared clastic dikes in the Dead Sea Basin [PDF]

, 2016
Peer ...
Alsop, G. I., Eyal, Y., Levi, T., Weinberger, R.   +3 more
core   +1 more source

Interseismic coupling and seismic potential along the Central Andes subduction zone [PDF]

, 2011
We use about two decades of geodetic measurements to characterize interseismic strain build up along the Central Andes subduction zone from Lima, Peru, to Antofagasta, Chile.
Aktug, Altamimi, Altamimi, Altamimi, Arriagada, Arriagada, Arriagada, Arriagada, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Audin, Baby, Baby, Baby, Baby, Baby, Baby, Baby, Baby, Barke, Barke, Barke, Barrientos, Barrientos, Barrientos, Bassin, Bassin, Bassin, Beck, Beck, Beck, Beck, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Bevis, Biggs, Biggs, Biggs, Bilek, Bilek, Brown, Brown, Brown, Brown, Béjar-Pizarro, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Bürgmann, Chen, Chen, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Chlieh, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Collot, Comte, Comte, Comte, Comte, Comte, Comte, Comte, Delouis, Delouis, Delouis, Delouis, DeMets, DeMets, DeMets, DeMets, Dominique Remy, Dorbath, Dorbath, Dorbath, Dragert, Dragert, Dragert, Engdhal, Engdhal, Engdhal, Farr, Farr, Francis Bondoux, Freymueller, Freymueller, Freymueller, Frédérique Rolandone, Gagnon, Gagnon, Gagnon, Germinal Gabalda, Giovanni, Giovanni, Giovanni, Hashimoto, Hashimoto, Hashimoto, Hashimoto, Haskell, Heki, Heki, Hernando Tavera, Hetland, Hetland, Hetland, Hindle, Hindle, Hindle, Hindle, Hindle, Hindle, Hirose, Hirose, Hirose, Hirose, Hirose, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hsu, Hu, Hu, Hu, Hu, Hu, Hugo Perfettini, Hyndman, Hyndman, Hyndman, Jean-Mathieu Nocquet, Jean-Philippe Avouac, Ji, Ji, Ji, Johnson, Johnson, Kanamori, Kanamori, Kanda, Kanda, Kaneko, Kaneko, Kaneko, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Kendrick, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Khazaradze, Kley, Kley, Konca, Lamb, Langer, Langer, Liu, Liu, Llenos, Llenos, Loveless, Loveless, Loveless, Loveless, Loveless, Loveless, Loveless, Lowry, Lowry, Lowry, Lowry, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, Massonnet, McQuarrie, McQuarrie, McQuarrie, Melnick, Melnick, Melnick, Melnick, Miyazaki, Miyazaki, Miyazaki, Mohamed Chlieh, Moreno, Moreno, Moreno, Motagh, Motagh, Motagh, Motagh, Motagh, Motagh, Motagh, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Norabuena, Oleskevich, Oleskevich, Oleskevich, Oncken, Oncken, Oncken, Oncken, Oncken, Oncken, Oncken, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Perfettini, Peyrat, Peyrat, Peyrat, Peyrat, Peyrat, Peyrat, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Pritchard, Robinson, Robinson, Robinson, Salichon, Salichon, Salichon, Salichon, Salichon, Salichon, Savage, Scholz, Sella, Sella, Sella, Silgado, Simons, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Sladen, Song, Song, Spence, Spence, Spence, Spence, Spence, Swenson, Swenson, Sylvain Bonvalot, Tavera, Tavera, Tavera, Tavera, Tavera, Tavera, Tavera, Thatcher, Tichelaar, Tichelaar, Vergne, Vergne, Vergne, Victor, Victor, Victor, Victor, Victor, Vigny, Vigny, Vigny, Vigny, Vigny, Vigny, Walker, Wallace, Wallace, Wallace, Wallace, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wang, Wells, Wells, Wells, Wells, Wells, Xie, Xie, Yoshioka, Yoshioka, Yoshioka, Yoshioka, Yoshioka, Yoshioka   +380 more
core   +5 more sources

The 2001 M_w 7.6 Bhuj earthquake, low fault friction, and the crustal support of plate driving forces in India [PDF]

, 2011
We present a source model for the 2001 M_w 7.6 Bhuj earthquake of northwest India. The slip distribution suggests a high stress drop (~35 MPa) and, together with the depth distribution of aftershocks, that the entire crust is seismogenic. We suggest that
Avouac, Jean-Philippe, Copley, Alex, Hollingsworth, James, Leprince, Sébastien   +3 more
core  

Coseismic and Postseismic Deformations of the 2023 Turkey Earthquake Doublet

Remote Sensing
On 6 February 2023, an earthquake doublet of Mw 7.8 and Mw 7.5 occurred in southeastern Turkey and caused surface ruptures over 350 km for the eastern Anatolian fault (EAF) and 150 km for the Surgu fault (SF), respectively. Over 3700 Mw > 3.0 aftershocks
Chaoya Liu, Hongru Li, Huili Zhan, Shaojun Wang, Ling Bai   +4 more
doaj   +1 more source

Investigation of a Seismic Intensity Prediction Model Using Multisource Observation Data Based on the LightGBM Method

IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
A revised version within the limit is provided below for your consideration. If the editorial office prefers to retain the current version, we are also fine with that.Revised abstract: Seismic intensity is a critical indicator for postearthquake damage ...
Yi Yu, Chengsheng Yang, Xue Li, Zhumei Liu, Xiaolin Chen   +4 more
doaj   +1 more source

Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake

Nature Communications, 2019
Large subduction zone earthquakes like the M 9.0 Tohoku earthquake of 2011 are followed by transient surface deformation. Here, the authors show this to be caused by rapid flow taking place in the asthenosphere due to temporarily decreased viscosity ...
Ryoichiro Agata, Sylvain D. Barbot, Kohei Fujita, Mamoru Hyodo, Takeshi Iinuma, Ryoko Nakata, Tsuyoshi Ichimura, Takane Hori   +7 more
doaj   +1 more source

Potential Inundation Hazards in the Taipei Basin Induced by Reactivation of the Shanchiao Fault in Northern Taiwan

Terrestrial, Atmospheric and Oceanic Sciences, 2010
The Shanchiao fault, located to the west of the Taipei Basin in northern Taiwan, is a highly active normal fault that has a left-slip component and fault length of over 40 km.
Jihn-Sung Lai, Chun-Ying Chiu, Hsiang-Kuan Chang, Jyr-Ching Hu, Yih-Chi Tan   +4 more
doaj   +1 more source