Current Status of Postseismic Deformation Following the 2011 Tohoku-Oki Earthquake
Postseismic deformation following the 2011 Tohoku-Oki earthquake has been observed by the Global Navigation Satellite System (GNSS) Earth Observation Network System (GEONET) and the Seafloor Geodetic Observation (SGO) over the past six and half years.
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Corrigendum: Gravity-driven postseismic deformation following the Mw 6.3 2009 L'Aquila (Italy) earthquake. [PDF]
Albano M +7 more
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Reconciling patterns of long-term topographic growth with coseismic uplift by synchronous duplex thrusting. [PDF]
Zhang Y +9 more
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The Mw 7.0 Dingri earthquake, the largest documented normal-faulting event in southern Tibet, struck within the NS-trending Dinggye-Xainza Rift system. Here we combine field observations, high resolution optical and synthetic aperture radar imagery and ...
Wenbin Xu +8 more
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Probing the seismic cycle timing with coseismic twisting of subduction margins. [PDF]
Corbi F +4 more
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Dislocation theory of steady and transient creep of crystalline solids: Predictions for olivine. [PDF]
Breithaupt T +3 more
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Increase in landslide activity after a low-magnitude earthquake as inferred from DInSAR interferometry. [PDF]
Martino S +5 more
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Seismic versus aseismic slip for the 2023 Kahramanmaraş earthquake doublet. [PDF]
Guo R +8 more
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Clustering Analysis Methods for GNSS Observations: A Data-Driven Approach to Identifying California's Major Faults. [PDF]
Granat R +9 more
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Metastable state preceding shear zone instability: Implications for earthquake-accelerated landslides and dynamic triggering. [PDF]
Li Y, Hu W, Xu Q, Luo H, Chang C, Jia X.
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