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Article . 2022 . Peer-reviewed
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Geological Society of America Bulletin
Article . 2012 . Peer-reviewed
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Chronostratigraphy of the Boltana anticline and the Ainsa Basin (southern Pyrenees)

Authors: Mochales López, Tania; Barnolas Cortina, Antonio; Pueyo Morer, Emilio Luis; Serra Kiel, J.; Casas-Sainz, Antonio M.; Samsó, Josep Maria; Ramajo, Javier; +1 Authors

Chronostratigraphy of the Boltana anticline and the Ainsa Basin (southern Pyrenees)

Abstract

The Ainsa Basin (south-central Pyrenees) is an exceptional example of a syntectonic foreland basin where structures oblique to the Pyrenean trend are well preserved. The absence of a complete chronostratigraphic frame motivated us to perform a detailed magnetostratigraphic study in the Ainsa Basin, including the shallow-marine–continental transition. Three sections covering almost the entire Eocene sedimentary fill were sampled (Ara, Coscollar, and Mondot), covering 2450 m of the sedimentary pile, with more than 1000 demagnetized specimens (sample spacing of 2.7 m). Data from previous magnetostratigraphic studies (Eripol section) allow us to complete the Eocene record with an 840-m-long profile within the Bartonian–Priabonian interval overlying the sampled sequence. Characteristic remanent magnetization (ChRM) directions were effectively isolated between 300 and 500 °C. Magnetite is the main magnetic carrier, with variable iron sulfide content and occasional hematite. Fold tests indicate a prefolding magnetization. Biostratigraphy based on shallow benthic foraminifera (15 localities) and a locality with abundant charophyte gyrogonites help to constrain the local magnetostratigraphic record (20 reversals) between the early Ilerdian and the middle Priabonian. A global correlation based on a magnetostratigraphic composite section derived from this work allows us to propose a complete chronostratigraphic frame for the Ainsa Basin infill between 55 and 45 Ma. Accumulation rates range from 2 to 53 cm/k.y., responding to retrogradational to progradational features during the early Lutetian, and a progressive increase from the middle Lutetian onward related to overall continentalization of the basin. Westward migration of subsidence is associated with progressively younger synsedimentary structures nucleating westward of the older ones in the South Pyrenean Basin Unidad de Zaragoza, Instituto Geológico y Minero de España, España Unidad de Tres Cantos, Instituto Geológico y Minero de España, España Departament d’Estratigrafia, Paleontologia i Geociències Marines, Universitat de Barcelona, España Departamento de Ciencias de la Tierra, Universidad de Zaragoza, España Consultant Geologist, España

Country
Spain
Keywords

anticlina, Pirineos Españoles, magnetoestratigrafía, cuenca antepaís, magnetita, Aínsa, bioestratigrafía, proceso sintectónico, Boltaña, Eoceno, cronoestratigrafía

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citations
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
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