Sedimentology of a Middle Jurassic Base-of-Slope environment, Cutri Formation, Mallorca


Autoria(s): Kettle, Simon Paul
Data(s)

07/06/2016

Resumo

The Cutri Formation’s, type location, exposed in the NW of Mallorca, Spain has previously been described by Álvaro et al., (1989) and further interpreted by Abbots (1989) unpublished PhD thesis as a base-of-slope carbonate apron. Incorporating new field and laboratory analysis this paper enhances this interpretation. From this analysis, it can be shown without reasonable doubt that the Cutri Formation was deposited in a carbonate base-of-slope environment on the palaeowindward side of a Mid-Jurassic Tethyan platform. Key evidence such as laterally extensive exposures, abundant deposits of calciturbidtes and debris flows amongst hemipelagic deposits strongly support this interpretation.

La Formación Cutri, en su localidad tipo en el noroeste de Mallorca (España), ha sido previamente interpretada como un posible prisma de talud carbonático. Esta interpretación es ratificada y pormenorizada en este trabajo con la incorporación de nuevos datos de campo y de laboratorio. El análisis realizado muestra que la Formación Cutri se depositó en la base del talud, en el lado de un ambiente carbonato de base de la pendiente a barlovento de una plataforma carbonatada tetisiana del Jurásico Medio. Esta interpretación está apoyada por extensos afloramientos de gran continuidad lateral, abundantes niveles de calciturbidtas y debris-flows entre los depósitos hemipelágicos.

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http://revistas.ucm.es/index.php/JIGE/article/view/50710

10.5209/rev_JIGE.2016.v42.n1.50710

Publicador

Ediciones Complutense

Relação

http://revistas.ucm.es/index.php/JIGE/article/view/50710/48546

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Fonte

Journal of Iberian Geology; Vol 42, No 1 (2016); 95-112

Journal of Iberian Geology; Vol 42, No 1 (2016); 95-112

Palavras-Chave #Science > Sedimentology #Calcilturbidte; Debrite; Bositra; Jurassic; Mallorca; Base-of-slope apron #calcilturbidita; debrita; Bositra; Jurásico; Mallorca; prisma de base de talud carbonático
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