RT Journal Article
T1 Secuencias deposicionales del Cretácico superior no terminal (Turoniense superior - Campaniense inferior) en la zona central de la Península Ibérica (Cordillera Ibérica y Sistema Central)
T1 Upper Cretaceous (Upper Turonian - Lower Campanian) Depositional Sequences in te Central Zone of the Iberian Peninsula (Iberian Ranges and Central Mountains)
A1 García, A.
A1 García Hidalgo, J. F.
A1 Segura, M.
A1 Gil, J.
A1 Carenas, B.
A1 Ruiz, G.
AB The Upper Cretaceous (Upper Turonian - Lower Campanian) in the central Iberian Peninsula is divided into 4 depositional sequences with an eustatic origin, which are correlated to the UZA 3-1 to UZA 3.4 of Haq et al. (1988) cycles chart, These sequences allow the establishment oí new temporal relationsships between well-known lithostratigraphic units. Tectonic also plays an important role both in the northwestwards shift of the Iberian basin during Upper Turonian -Lower Coniacian; and in the intra-Santonian events: an angular unconformity in the south border of the Central Mountains and a southeastwards shift in the basin allowing a brief Tethys - Atlantic connection
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/11430
UL http://hdl.handle.net/10272/11430
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026