Intercalación de un sistema turbidítico siliciclástico entre carbonatos de plataforma: implicaciones tectónicas (Aptiense-Albiense, cabo Ogoño, Bizkaia)
A turbidite siliciclastic system between platform carbonates: tectonic implications (Aptian-Albian, cape Ogoño, Bizkaia)
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Publication Date
1991 -
Publisher
Sociedad Geológica de España -
Abstract
A turbidite (channel-levee) siliciclastic system replaced vertically a mixed carbonate and terrigenous platform, and it in turn was replaced by litoral sandstones and bank carbonates (Aptian-Albian, Ogoño, Bizkaia). An E-W composite stratigraphical section shows that an inversion in subsidence tool< place approximate/y around the Ibarrangelua N-S paleogeographic line during the process. Therefore, the action ofa deep-seated, probab/y wrench fau/t is invoked to account for the origin ofthe turbidite system in this unusual context
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Intercalacion.pdf | 329.8Kb | View/ | There is no description for this item |
Fichero | Tamaño | Formato |
| Description |
---|---|---|---|---|
Intercalacion.pdf | 329.8Kb | View/ | There is no description for this item |