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- W2999696852 abstract "Abstract The removal, redistribution, and transient storage of sediments in tectonically active mountain belts is thought to exert a first-order control on shallow crustal stresses, fault activity, and hence on the spatiotemporal pattern of regional deformation processes. Accordingly, sediment loading and unloading cycles in intermontane sedimentary basins may inhibit or promote intrabasinal faulting, respectively, but unambiguous evidence for this potential link has been elusive so far. Here we combine 2D numerical experiments that simulate contractional deformation in a broken-foreland setting (i.e., a foreland where shortening is diachronously absorbed by spatially disparate, reverse faults uplifting basement blocks) with field data from intermontane basins in the NW Argentine Andes. Our modeling results suggest that thicker sedimentary fills (>0.7–1.0 km) may suppress basinal faulting processes, while thinner fills (" @default.
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- W2999696852 date "2018-04-01" @default.
- W2999696852 modified "2023-09-24" @default.
- W2999696852 title "Sedimentary loading-unloading cycles and faulting in intermontane basins: insights from numerical modeling and field observations in the NW Argentine Andes" @default.
- W2999696852 hasPublicationYear "2018" @default.
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