RT Journal Article
T1 El Albense - Cenomanense medio de la Sierra de Altomira
T1 The Albian- Middle Cenomanian ofthe Altomira Mountains
A1 Carenas, B.
A1 García Palacios, A.
A1 Segura, M.
A1 García Hidalgo, J. F.
AB The Cretaceous transgression in the Sierra de Altomira starts with sandy (Utrillas Fm.) and dolomitic sediments (Villa de Ves Mb.), its detailed sequential analysis allow the recognition of five depositional sequences with a progressively less thickness from base to top: the basal sequence is terrigenous, appearing only in the north, it represents fluvial sediments. The second one is terrigenous in northern and southern areas, meanwhile it is dolomitic in the central area, it is interpreted as deposited in littoral environments. The 3rd and 4th sequences are composed by tidal flats dolostones. And finally, the upper sequence is composed of shallow dolostones, with a southwards decreasing thicknesses
PB Sociedad Geológica de España
YR 1993
FD 1993
LK http://hdl.handle.net/10272/14027
UL http://hdl.handle.net/10272/14027
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026