La situación estratigráfica de las “margas de Bañolas” (Almela y Ríos 1943)

descriptionPublicationkeyboard_double_arrow_right Article 01 Jan 1970 Spain Spanish Publisher:CSIC - Instituto de Ciencias de la Tierra Jaume Almera (ICTJA)Journal:Acta geológica hispánica

Authors: CLAVELL I VERGÉS, Eduard; DEFALQUE, GÉRARD; REGUANT, SALVADOR;

handle: 10261/7934 , 2445/32774

La situación estratigráfica de las “margas de Bañolas” (Almela y Ríos 1943)

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Abstract

[ES] Se demuestra que las "margas de Bañolas" (Almela y Rios 1943) y las margas que se sitúan encima de la "caliza de Tavertet" (Reguant 1967) entre Vic y El Far son dos formaciones distintas. Estas últimas que se pueden llamar "margas de El Coll de Malla", son de edad Biarritzense inferior, mientras que las "margas de Bañolas" son posiblemente del Luteciense inferior o medio.

[EN] The "margas de Bañolas" (Almela Y Ríos 1943) and the marls that are placed above the "caliza de Tavertet" (Reguant 1967) in Vic-El Far region, are two distinct formations. Thece marls could be named "mareas de El Coll de Malla", and are from the Lower Biarritzian. The "margas de Bañolas" are from the Lower or Middle Lutetian.

Peer reviewed

Country

Spain

Related Organizations

University of Barcelona
Spain

Keywords

Estratigrafia, Banyoles (Catalonia), Banyoles (Catalunya), Margas de Bañolas, Stratigraphic geology

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