La Formación Marín: redepósito de material jurásico durante el Mioceno (zona Subbética)
An important volume about resedimented materials during the Burdigalian has been confused with the oolite Dogger even today. This article determines the Marin Formation, litostratigraphic unit that includes these rocks. It will be caracterized by the prevalence of the conglomeratic beds (A facies),...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | Spanish |
Published: |
Sociedad Geológica de España
1990
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Subjects: | |
Online Access: | http://hdl.handle.net/10272/18188 |