RT Journal Article
T1 Calizas oolíticas entre facies pelágicas en el Jurásico medio de Iznájar (Prov. de Córdoba, Subbético): significado paleogeográfico y paleobati métrico
T1 Oolitic limestones between pelagic facies in the Middle Jurassic from Iznajar Cordoba province, Subbetic): palaeogeographic and palaeobathymetric significance
A1 Vera, J. A.
A1 Molina, José Miguel
AB On the top of the Zegrí Fm (Aalenian-Bajocian) oí the Median Subbetic in the Iznajar area (south of the Córdoba province) oolitic limestones outcrop, interbedded between pelagic facies. These oolitic limestones were previously interpreted as calcareous turbidites. The detailed study of their microfacies, stratigraphic location, geometry of the sedimentary beds and sedimentary structures has allowed us to interpret these limestones as deposited in isolated carbonate platforms similar to the recognized in other areas of the Median Subbetic. This interpretation asserts that the overlying and underlying pelagic sediments were deposited (o a moderate depth (some hundreds of meters)
PB Sociedad Geológica de España
YR 2001
FD 2001
LK http://hdl.handle.net/10272/9511
UL http://hdl.handle.net/10272/9511
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026