Tectonic deformation along the External Dinarides fold-and-thrust belt is slow, with transpressional crustal strain redistributed along multiple faults. Some of these faults reach the surface along ...
Evaluation of landforms, soils, and deposits formed by active tectonics is providing basic data necessary for long-term earthquake prediction, seismic-hazard evaluation, and probabilistic seismic-risk ...
Strike-slip fault systems arise where lateral shear stress dominates, causing crustal blocks to slide past one another. Along such faults, bends and step-overs generate zones of transpression ...
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