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Spanning the Arc: Margin Geometry and Topography Control Upper Plate Deformation in the Central Andean Subduction Zone

Subduction zone forearcs deform transiently and permanently due to the frictional coupling with the converging lower plate. Transient stresses are mostly the elastic response to the seismic cycle. Permanent deformation is evidenced by forearc topography, upper plate faulting, and earthquakes; its relation to the megathrust seismic cycle is debated ...
Bernd Schurr   +3 more
openaire   +1 more source

Research on the mechanism of asymmetric deformation and stability control of near-fault roadway under the influence of mining

, 2021
Renliang Shan   +6 more
semanticscholar   +1 more source

Coordinated deformation control technologies for the high sidewall—bottom transfixion zone of large underground hydro-powerhouses

Journal of Zhejiang University-SCIENCE A, 2022
Qi-xiang Fan   +5 more
openaire   +1 more source

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