Detachment fold vs. ramp anticline: A gravity survey in the southern Pyrenean front (External Sierras)
Resumen: The Santo Domingo Anticline (External Sierras, Southern Pyrenees), which separates the Jaca piggyback basin from the Ebro foreland basin, is a key structure of the Pyrenees. Its geometry has been interpreted both as a detachment fold and as a hangingwall anticline associated with an underlying thrust. In this paper, we present the results from a gravity survey and 2.5D gravity modelling carried out around the Santo Domingo Anticline. Density measurements indicate a sharp density contrast between the Triassic evaporites-mudstones in the core of the anticline and the sedimentary sequence (limestones and sandstones) at its limbs. Gravity anomalies together with 2.5D gravity models allow to discern the along-strike structural changes. From east to west, we document a change from the ramp-associated fold to the detachment anticline. The capabilities and limitations of the gravimetric method for the determination of fold geometry are also discussed.
Idioma: Inglés
DOI: 10.1002/gj.2884
Año: 2017
Publicado en: GEOLOGICAL JOURNAL 53, 1 (2017), 178-190
ISSN: 0072-1050

Factor impacto JCR: 1.654 (2017)
Categ. JCR: GEOSCIENCES, MULTIDISCIPLINARY rank: 110 / 189 = 0.582 (2017) - Q3 - T2
Factor impacto SCIMAGO: 0.846 - Geology (Q2)

Financiación: info:eu-repo/grantAgreement/ES/MINECO/CGL2014-54118-C2
Tipo y forma: Article (PostPrint)
Área (Departamento): Área Geodinámica Interna (Dpto. Ciencias de la Tierra)
Exportado de SIDERAL (2026-02-19-14:10:43)


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articulos > articulos-por-area > geodinamica_interna



 Notice créée le 2026-02-19, modifiée le 2026-02-19


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