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2003

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Please use this identifier to cite or link to this item: https://hdl.handle.net/2445/34427

Tectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain)

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Abstract

Two small, alluvial-lacustrine subbasins developed during the early restraining overstep stages of the Oligocene-Miocene As Pontes strike-slip Basin (NW Spain). Later, the basin evolved into a restraining bend stage and an alluvial-swamp-dominated depositional framework developed. The palaeobiological record demonstrates that the Oligocene-Miocene palaeoclimate in NW Spain was subtropical, warm and humid to subhumid.

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Sediments fluvials, Oligocè, Miocè, Espanya

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River sediments, Oligocene, Miocene, Spain

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Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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SÁEZ, Alberto, et al. Tectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain). Sedimentary Geology. 2003. Vol. 159, num. 3-4, pags. 305-324. ISSN 0037-0738. [consulted: 17 of June of 2026]. Available at: https://hdl.handle.net/2445/34427

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