The Upper Devonian of the river Sil area: a stratigraphic correlation between León and Asturias, northern Spain

Authors

  • G. B. S. van Loevezijn
  • J. G. M. Raven Naturalis Biodiversity Center Leiden

DOI:

https://doi.org/10.21701/bolgeomin.132.3.005

Keywords:

Cantabrian Mountains, depositional history, facies, sequence stratigraphy, Upper Devonian

Abstract


We have studied the Upper Devonian succession of the river Sil area divided into five sections along a SW-NE transect. Thirteen lithofacies types have been identified based on lithology and sedimentological structures. They have been organised into facies associations representing depositional environments from the fluviomarine zone of the nearby part of the basin towards the distal offshore zone. Erosion surfaces and sequence boundaries have been identified and the succession is connected to the Upper Devonian sequence stratigraphic model of the southern Cantabrian Mountains and the Upper Devonian succession of the Coastal Ranges of Asturias in the north. The main portion of the Upper Devonian succession of the Sil area can be correlated with the Nocedo Formation, Gordón Member (sequence A) of early Frasnian age. In the south-westernmost sections of the Sil area parts of the Fueyo and Ermita formations are exposed; they constitute sequence C of early Famennian age. The Upper Devonian Unconformity separates these thick Frasnian-Famennian coarsening upward sequences from the overlying extensive Famennian-Tournaisian condensed succession of the Llombera Beds (sequence D).

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2021-09-30

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van Loevezijn, G. B. S. ., & Raven, J. G. M. (2021). The Upper Devonian of the river Sil area: a stratigraphic correlation between León and Asturias, northern Spain. Boletín Geológico Y Minero, 132(3), 325–354. https://doi.org/10.21701/bolgeomin.132.3.005

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