NDLI: Pulsos de inundación marina en la terminación de una plataforma carbonatada (Aptiense inferior de Aralar, Cuenca Vasco-Cantábrica)

Content Provider	Semantic Scholar
Author	Millán, María Isabel Pérez Mendiola, Pedro Angel Fernández Mondéjar, Joaquín García
Copyright Year	2006
Abstract	The Lower Aptian Sarastarri Limestone unit (Aralar, nor thern Spain), mainly consists of rudist and coral micrites and is nearly 200m thick. The uppermost 30m of the unit show sharp-based marly intervals attributed to two drowning events. Both marly intervals are immediately preceeded by laminated bioclastic rudstone facies, attributed to quick shoaling processes ending with subaerial exposure. A change of local subsidence conditions from uniform during the Sarastarri Limestone episode, to varying with distance during the Lareo Marl succeeding episode, is invoked to explain both drownings. Influence of oceanographic causes reported in other contemporaneous carbonate platforms is, however, not excluded.
Starting Page	127
Ending Page	130
Page Count	4
File Format	PDF HTM / HTML
Alternate Webpage(s)	http://www.sociedadgeologica.es/archivos/geogacetas/Geo41/G41Art32.pdf
Alternate Webpage(s)	http://rabida.uhu.es/dspace/bitstream/handle/10272/8523/Pulsos.pdf?sequence=2
Language	English
Access Restriction	Open
Content Type	Text
Resource Type	Article

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