2009
DOI: 10.1007/s10347-009-0203-7
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From ramp to platform: building a 3D model of depositional geometries and facies architectures in transitional carbonates in the Miocene, northern Sardinia

Abstract: The depositional geometry and facies distribution of an Early Miocene (Burdigalian) carbonate system in the Perfugas Basin (NW Sardinia) comprise a well-exposed example of a transition from a ramp to a steep-flanked platform. The carbonate succession (Sedini Limestone Unit) is composed of two depositional sequences separated by a major erosional unconformity. The lower (sequence 1) records a ramp dominated by heterozoan producers and the upper (sequence 2) is dominated by photozoan producers and displays a gra… Show more

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Cited by 18 publications
(4 citation statements)
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“…However, the combination of different GPS data sets, collected at different times or with different acquisition methods, may show an offset (vertical and/or horizontal) between one data set and another (Verwer et al. , 2007; Tomás et al. , 2010).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…However, the combination of different GPS data sets, collected at different times or with different acquisition methods, may show an offset (vertical and/or horizontal) between one data set and another (Verwer et al. , 2007; Tomás et al. , 2010).…”
Section: Methodsmentioning
confidence: 99%
“…The last category mixes several modelling methodologies in their simulation workflow (Palermo et al. , 2010; Tomás et al. , 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Diversos estudios en plataformas carbonatadas similares han puesto de manifiesto la compleja distribución que presentan las facies en este tipo de ambientes, consecuencia de la actuación de diversos procesos tanto internos como externos a la plataforma (e.g., Rankey, 2002;Strasser y Védrine, 2007). Asimismo, los componentes que definen un determinado cinturón de facies pueden variar lateralmente de manera significativa, e incluso desarrollarse mosaicos de facies en determinadas zonas de la plataforma (e.g., Bádenas et al, 2010;Tomás et al, 2010;Amour et al, 2013;San Miguel et al, 2017;Tomassetti et al, 2018). De cara a la obtención de modelos sedimentarios más precisos que reflejen el funcionamiento de estos sistemas carbonatados, el principal objetivo de este trabajo consiste en caracterizar en detalle la distribución de facies y evolución sedimentaria de las zonas someras de una rampa carbonatada de finales del Kimmeridgiense, representada en los materiales de la Fm.…”
Section: Introducción Y Objetivosunclassified
“…Digital outcrop models (DOMs) help to better understand the geometries of complex carbonate depositional systems and their internal facies architecture (Bellian et al, 2005;Warrlich et al, 2005;Tom as et al, 2009;Verwer et al, 2009;Benson et al, 2014). Digital outcrop models can be integrated with field observations, laboratory data, high-detail photographs and GPS (global positioning system) data to create three-dimensional geological models.…”
Section: Introductionmentioning
confidence: 99%