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Tectonic and morphosedimentary features of the 2010 Chile earthquake and tsunami in the Arauco Gulf and Mataquito River (Central Chile)
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文摘

Land deformation, run up, inundation extent and deposit extent and thickness were measured in the field after the earthquake.

Coseismic deformation measured by means of bio- and geomorphic markers agrees both with model deformation and measured GPS.

No relationship was found between coseismic land deformations, tsunami run-up and sedimentological features.

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