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- W2584851318 abstract "Subduction of the Nazca plate under the peruvian and chilean segments of the Andes is associated with variable characteristic structures of the corresponding forearc. The forearc constitutes this specifie zone recognised to deform slowly (of the order of 1mm/yr or less according to different sources), squeezed inbetween the oceanic plate subducting at around 8 cm/yr, and the growing Andes that thicken the border of the South American continent. Depending on its latitud inal pos ition , as weil as in east-west directions, this forearc has developped numerous features of either extensional or inverse signature, sometimes co-eval: the coastal escarpment (coastal cordillera), the Central Depression, or the Atacama fault zone, are only some of the most proeminant yet still enigmatic structures that compose the chilean forearc." @default.
- W2584851318 created "2017-02-10" @default.
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- W2584851318 date "2005-01-01" @default.
- W2584851318 modified "2023-09-27" @default.
- W2584851318 title "Normal faulting in a forearc submitted to slab pull: Numerical models and insight on the structure of the Chilean forearc" @default.
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