000126429 001__ 126429
000126429 005__ 20241125101138.0
000126429 0247_ $$2doi$$a10.1111/sed.13097
000126429 0248_ $$2sideral$$a133935
000126429 037__ $$aART-2023-133935
000126429 041__ $$aeng
000126429 100__ $$0(orcid)0000-0003-2963-8422$$aSoria, Ana R.$$uUniversidad de Zaragoza
000126429 245__ $$aSedimentology and stratigraphic architecture of Barremian synrift barrier island–estuarine depositional systems from blended field and drone-derived data
000126429 260__ $$c2023
000126429 5060_ $$aAccess copy available to the general public$$fUnrestricted
000126429 5203_ $$aThe 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.
000126429 536__ $$9info:eu-repo/grantAgreement/ES/AEI/PID2019-108705GB-I00$$9info:eu-repo/grantAgreement/ES/DGA/E32-20R
000126429 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000126429 590__ $$a2.6$$b2023
000126429 592__ $$a1.289$$b2023
000126429 591__ $$aGEOLOGY$$b6 / 61 = 0.098$$c2023$$dQ1$$eT1
000126429 593__ $$aStratigraphy$$c2023$$dQ1
000126429 593__ $$aGeology$$c2023$$dQ1
000126429 594__ $$a8.2$$b2023
000126429 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000126429 700__ $$0(orcid)0000-0002-9130-117X$$aLiesa, Carlos L.$$uUniversidad de Zaragoza
000126429 700__ $$0(orcid)0000-0002-7739-6096$$aNavarrete, Rocío
000126429 700__ $$aRodríguez-López, Juan Pedro
000126429 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000126429 7102_ $$12000$$2428$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Geodinámica Interna
000126429 773__ $$g70, 6 (2023), 1812–1855$$pSedimentology$$tSEDIMENTOLOGY$$x0037-0746
000126429 8564_ $$s2890090$$uhttps://zaguan.unizar.es/record/126429/files/texto_completo.pdf$$yVersión publicada
000126429 8564_ $$s2347015$$uhttps://zaguan.unizar.es/record/126429/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000126429 909CO $$ooai:zaguan.unizar.es:126429$$particulos$$pdriver
000126429 951__ $$a2024-11-22-12:01:46
000126429 980__ $$aARTICLE