@article{10272/8404,
year = {2007},
url = {http://hdl.handle.net/10272/8404},
abstract = {The upper Neogene deposits which outcrop in the area of Vejer de la Frontera (Cádiz, SW Spain) have
been studied. The sedimentological, paleontological, and taphonomic changes, suggest a progressive
phenomenon of upward regression, in a carbonate-detrital ramp context. Deposition begins with outer
shelf sandy marls which change to calcarenites interpreted as inner shelf submareal bars and belong to the
Foramol assemblage. Finally, conglomerates with marine fauna are deposited and this points to litoral
environment systems},
title = {El Neógeno superior marino en Vejer de la Frontera (Cádiz, SO España) y su evolución regresiva},
title = {Upper Neogene marine deposits in Vejer de la Frontera site (Cádiz, SW Spain) and their regressive evolution},
author = {Rico García, Alberto},
}