Publications des scientifiques de l'IRD

Encinas A., Finger K. L., Nielsen S. N., Lavenu Alain, Buatois L. A., Peterson D. E., Le Roux J. P. (2008). Rapid and major coastal subsidence during the late Miocene in south-central Chile. Journal of South American Earth Sciences, 25 (2), p. 157-175. ISSN 0895-9811.

Titre du document
Rapid and major coastal subsidence during the late Miocene in south-central Chile
Année de publication
2008
Type de document
Article référencé dans le Web of Science WOS:000255082400003
Auteurs
Encinas A., Finger K. L., Nielsen S. N., Lavenu Alain, Buatois L. A., Peterson D. E., Le Roux J. P.
Source
Journal of South American Earth Sciences, 2008, 25 (2), p. 157-175 ISSN 0895-9811
Sedimentological and paleontological studies, including foraminifera, ostracodes, gastropods, and trace fossils, were carried Out on Neogene sedimentary successions and offshore boreholes of south-central Chile (similar to 33 degrees-45 degrees S). Sedimentology shows the occurrence of a thin, shallow marine, basal conglomerate overlain by a succession that includes the following facies: massive sandstones, conglomerates, interbedded siltstones and sandstones showing Bouma cycles, parallel-laminated sandstones, synsedimentary breccias, slides, slumps, diamictites, and massive siltstones. These facies were deposited by gravity flows, with turbidity currents and sandy debris flows as the main modes of deposition. Paleontology indicates the occurrence of trace fossils assigned to the Zoophycos ichnofacies and deep-water (similar to 2000 m) benthic foraminifers, ostracodes, and gastropods. Sedimentology and paleontology indicate that deposition took place on a slope apron during a period of rapid and major forearc subsidence. Planktic foraminifers indicate ages ranging from the late Miocene to the early Pliocene (zones N16-N19) for these successions. We attribute this episode of major Neogene subsidence to an important event of subduction erosion that would have retrieved the underside of the upper continental plate and caused its thinning.
Plan de classement
Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010042545]
Identifiant IRD
fdi:010042545
Contact
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