Tectono-stratigraphic evolution of an inverted extensional basin: the Cameros Basin (north of Spain)
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- 作者：Silvia Omodeo Salè (1)
Joan Guimerà (2)
Ramón Mas (3)
José Arribas (1) - 关键词：Extensional synclinal basin ; Syn ; rift geometry and architecture ; Tectono ; stratigraphic evolution ; Iberian rift ; Inverted basin
- 刊名：International Journal of Earth Sciences
- 出版年：2014
- 出版时间：September 2014
- 年：2014
- 卷：103
- 期：6
- 页码：1597-1620
- 全文大小：11,315 KB
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Joan Guimerà (2)
Ramón Mas (3)
José Arribas (1)
1. Dpto. Petrología y Geoquímica, Facultad de Ciencias Geológicas, UCM-IGEO (CSIC), José Antonio Novais, 12, 28040, Madrid, Spain
2. Dpt. Geodinàmica i Geofísica, Universitat de Barcelona, Martí i Franqués s/n, 08028, Barcelona, Spain
3. Dpto. Estratigrafía, Facultad de Ciencias Geológicas, UCM-IGEO (CSIC), José Antonio Novais, 12, 28040, Madrid, Spain - ISSN：1437-3262
文摘
The Cameros Basin is a part of the Mesozoic Iberian Rift. It is an extensional basin formed during the late Jurassic and early Cretaceous, in the Mesozoic Iberian Rift context, and it was inverted in the Cenozoic as a result of the Alpine contraction. This work aims to reconstruct the tectono-stratigraphic evolution of the basin during the Mesozoic, using new and revised field, geophysical and subsurface data. The construction of a basin-wide balanced section with partial restorations herein offers new insights into the geometry of the syn-rift deposits. Field data, seismic lines and oil well data were used to identify the main structures of the basin and the basin-forming mechanisms. Mapping and cross-sectional data indicate the marked thickness variation of the depositional sequences across the basin, suggesting that the extension of the depositional area varied during the syn-rift stage and that the depocentres migrated towards the north. From field observation and seismic line interpretation, an onlap of the depositional sequences to the north, over the marine Jurassic substratum, can be deduced. In the last few decades, the structure and geometry of the basin have been strongly debated. The structure and geometry of the basin infill reconstructed herein strongly support the interpretation of the Cameros Basin as an extensional-ramp synclinal basin formed on a blind south-dipping extensional ramp. The gradual hanging-wall displacement to the south shifted the depocentres to the north over time, thus increasing the basin in size northwards, with onlap geometry on the pre-rift substratum. The basin was inverted by means of a main thrust located in a detachment located in the Upper Triassic beds (Keuper), which branched in depth with the Mesozoic extensional fault flat. The reconstruction of the tectono-stratigraphic evolution of the Cameros Basin proposed herein represents a synthesis and an integration of previous studies of the structure and geometry of the basin. This study can be used as the basis for future basin-scale research and for modelling the ancient petroleum system of the basin.