@article{10272/11430,
year = {1996},
url = {http://hdl.handle.net/10272/11430},
abstract = {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},
publisher = {Sociedad Geológica de España},
keywords = {Upper Cretaceous},
keywords = {Depositional sequences},
keywords = {Central Mountains},
keywords = {Iberian Ranges},
keywords = {Spain},
title = {Secuencias deposicionales del Cretácico superior no terminal (Turoniense superior - Campaniense inferior) en la zona central de la Península Ibérica (Cordillera Ibérica y Sistema Central)},
title = {Upper Cretaceous (Upper Turonian - Lower Campanian) Depositional Sequences in te Central Zone of the Iberian Peninsula (Iberian Ranges and Central Mountains)},
author = {García, A. and García Hidalgo, J. F. and Segura, M. and Gil, J. and Carenas, B. and Ruiz, G.},
}