Sedimentology and stratigraphic architecture of Barremian synrift barrier island–estuarine depositional systems from blended field and drone-derived data
Resumen: The Lower Cretaceous (Barremian) Camarillas Formation in the Galve Sub-basin of eastern Spain is an exceptionally muddy, synrift, aggradational then retrogradational paralic succession. Deposition within these arid, equatorial paralic systems was strongly controlled by crustal rifting of the Iberia plate linked to the geodynamic evolution of the Atlantic Ocean, the Bay of Biscay and the Tethys Ocean. Although synsedimentary extensional tectonics controlled thickness and facies distributions, the parasequence stacking patterns point to a superimposed high-order allogenic control on the paralic succession. Field data and drone imagery are combined to document changes in sedimentology and three-dimensional stratigraphic architecture of these deposits to interpret changes in depositional environments as this basin filled. Three evolutionary stages are identified: (i) tide-dominated estuary; (ii) mixed-energy estuary, with a well-developed wave-dominated barrier island system; and (iii) barrier island–tidal inlet suite. An exceptional record of back-barrier-island depositional interactions is preserved in this high-subsidence, extensional-basin setting, including deposition of washover fans, flood-tidal deltas and ebb-tidal deltas. Drone-derived imagery facilitates three-dimensional architectural characterization of these complex paralic deposits, including multi-episodic tidal inlets, and correlation of basin scale stratigraphic markers. Spatio-temporal interactions between climate change, sea-level variations and rift-related subsidence generated complex estuarine and barrier island geobodies. The general transgressive trend recorded in the Camarillas Formation correlates well with global eustatic sea-level rise during the Barremian.
Idioma: Inglés
DOI: 10.1111/sed.13097
Año: 2023
Publicado en: SEDIMENTOLOGY 70, 6 (2023), 1812–1855
ISSN: 0037-0746

Factor impacto JCR: 2.6 (2023)
Categ. JCR: GEOLOGY rank: 6 / 61 = 0.098 (2023) - Q1 - T1
Factor impacto CITESCORE: 8.2 - Geology (Q1) - Stratigraphy (Q1)

Factor impacto SCIMAGO: 1.289 - Stratigraphy (Q1) - Geology (Q1)

Financiación: info:eu-repo/grantAgreement/ES/AEI/PID2019-108705GB-I00
Financiación: info:eu-repo/grantAgreement/ES/DGA/E32-20R
Tipo y forma: Article (Published version)
Área (Departamento): Área Estratigrafía (Dpto. Ciencias de la Tierra)
Área (Departamento): Área Geodinámica Interna (Dpto. Ciencias de la Tierra)

Exportado de SIDERAL (2024-11-22-12:01:46)


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Este artículo se encuentra en las siguientes colecciones:
articulos > articulos-por-area > geodinamica_interna
articulos > articulos-por-area > estratigrafia



 Notice créée le 2023-06-21, modifiée le 2024-11-25


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