@article{10272/9377,
year = {2002},
url = {http://hdl.handle.net/10272/9377},
abstract = {Calcareous breccias from Antolin (Guadiato Área, Córdoba Province) have been analysed. Paleontological and sedimentological studies of those breccias, allowed a reconstruction of a not-preserved calcareous platform or ramp. Breccias from Antolin show six types of clasts and blocks: oolithic grainstones originated in calcareous shoals, coral-algal boundstones originated in patch-reefs, packstones that are mainly composed of solitary corals and brachiopods produced in shallow quiet waters, crinoidal packstones originated in crinoida! prairies, mudstones-wackestones with micropeloidal and cryptalgal textures that were originated in mud mounds and calcareous sandstones originated in a mixed ramp.

The debris flow was located in the photic zone of a middle, mixed ramp, because clasts show algal and bryozoan crusts; moreover, clasts and blocks show signs of short transportation},
publisher = {Sociedad Geológica de España},
title = {Reconstrucción de una plataforma carbonatada Viseense no preservada en el Área del Guadiato (Córdoba, SO de España)},
title = {Reconstruction of a non-preserved Viséan calcareous platform in the Guadiato Area(Córdoba, SW Spain)},
author = {Rodríguez, Sergio and Rodríguez Curt, L.},
}