Earthquake cycle deformation and the Moho: Implications for the rheology of continental lithosphere
The last 20 years has seen a dramatic improvement in the quantity and quality of geodetic
measurements of the earthquake loading cycle. In this paper we compile and review these …
measurements of the earthquake loading cycle. In this paper we compile and review these …
Dominant Controls of Downdip Afterslip and Viscous Relaxation on the Postseismic Displacements Following the Mw7.9 Gorkha, Nepal, Earthquake
B Zhao, R Bürgmann, D Wang, K Tan… - Journal of …, 2017 - Wiley Online Library
We analyze three‐dimensional GPS coordinate time series from continuously operating
stations in Nepal and South Tibet and calculate the initial 1 year postseismic displacements …
stations in Nepal and South Tibet and calculate the initial 1 year postseismic displacements …
Probing the lithospheric rheology across the eastern margin of the Tibetan Plateau
The fundamental geological structure, geodynamics, and rheology of the Tibetan Plateau
have been debated for decades. Two end-member models have been proposed:(1) the …
have been debated for decades. Two end-member models have been proposed:(1) the …
Geodynamic complexity of the Indo-Burmese Arc region and its interaction with Northeast Himalaya
Abstract The Indo-Burmese Arc (IBA) comprises highly populated regions of Northeast India,
Bangladesh, and Myanmar. Thus, quantitative estimation of crustal deformation, earthquake …
Bangladesh, and Myanmar. Thus, quantitative estimation of crustal deformation, earthquake …
Fault behavior and lower crustal rheology inferred from the first seven years of postseismic GPS data after the 2008 Wenchuan earthquake
Long-term and wide-area geodetic observations may allow identifying distinct postseismic
deformation processes following large earthquakes, and thus can reveal fault behavior and …
deformation processes following large earthquakes, and thus can reveal fault behavior and …
Kinematic fault slip evolution source models of the 2008 M7. 9 Wenchuan earthquake in China from SAR interferometry, GPS and teleseismic analysis and …
Abstract The M w 7.9 2008 Wenchuan earthquake ruptured about 280 km of faults in the
Longmen Shan of Sichuan province, China, at the eastern edge of the Tibetan Plateau. We …
Longmen Shan of Sichuan province, China, at the eastern edge of the Tibetan Plateau. We …
Lower crustal relaxation beneath the Tibetan Plateau and Qaidam Basin following the 2001 Kokoxili earthquake
Summary In 2001 November a magnitude 7.8 earthquake ruptured a 400 km long portion of
the Kunlun fault, northeastern Tibet. In this study, we analyse over five years of post-seismic …
the Kunlun fault, northeastern Tibet. In this study, we analyse over five years of post-seismic …
Postseismic motion after the 2001 MW 7.8 Kokoxili earthquake in Tibet observed by InSAR time series
On November 14th 2001, a Mw 7.8 earthquake occurred in the Kokoxili region of northern
Tibet. The earthquake ruptured more than 400 km along the western part of the Kunlun fault …
Tibet. The earthquake ruptured more than 400 km along the western part of the Kunlun fault …
Spatio-temporal variations of afterslip and viscoelastic relaxation following the Mw 7.8 Gorkha (Nepal) earthquake
Z Tian, JT Freymueller, Z Yang - Earth and Planetary Science Letters, 2020 - Elsevier
We use 4 years of 3D GPS data from Nepal and southern Tibet to investigate the
postseismic deformation caused by the 2015 M w 7.8 Gorkha (Nepal) earthquake. We first …
postseismic deformation caused by the 2015 M w 7.8 Gorkha (Nepal) earthquake. We first …
Large extensional aftershocks in the continental forearc triggered by the 2010 Maule earthquake, Chile
I Ryder, A Rietbrock, K Kelson… - Geophysical Journal …, 2012 - academic.oup.com
The M w 8.8 Maule earthquake occurred off the coast of central Chile on 2010 February 27
and was the sixth largest earthquake to be recorded instrumentally. This subduction zone …
and was the sixth largest earthquake to be recorded instrumentally. This subduction zone …