2013
DOI: 10.1016/j.tecto.2013.02.012
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Seismic structure and tectonics of the southern Arauco Basin, south-central Chile (~38°S)

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Cited by 24 publications
(23 citation statements)
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“…This variation is determined by a number of morphostructural systems from west to east ( Figure 3A): i) Offshore basins developed over the Chilean forearc, are encompassing a series of extensional depocenters up to 4,000 m thick developed from latest Cretaceous to Quaternary times (González, 1989;Radic et al, 2009;Becerra et al, 2013).…”
Section: Structure and Exhumation Of The Fold And Thrust Belt Betweenmentioning
confidence: 99%
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“…This variation is determined by a number of morphostructural systems from west to east ( Figure 3A): i) Offshore basins developed over the Chilean forearc, are encompassing a series of extensional depocenters up to 4,000 m thick developed from latest Cretaceous to Quaternary times (González, 1989;Radic et al, 2009;Becerra et al, 2013).…”
Section: Structure and Exhumation Of The Fold And Thrust Belt Betweenmentioning
confidence: 99%
“…First sedimentation at the offshore region started in Early-Late Cretaceous times controlled by extension (Becerra et al, 2013) that passes to non-marine sections over the retroarc zone that show synorogenic characteristics (Tunik et al, 2010). Paleocene to Eocene sections at the Pacific offshore region and Central Valley area are controlled by normal faults (Becerra et al, 2013), while to the east over the axial Andes and retroarc region arc-related rocks are present (Suárez and Emparán, 1997) with an unknown mechanics of formation.…”
Section: Structure and Exhumation Of The Fold And Thrust Belt Betweenmentioning
confidence: 99%
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