RT Journal Article
T1 Evolución y estructuras alpinas en la zona del centro peninsular
T2 Alpine structure and evolution of central Spain
A1 Vicente Muñoz, Gerardo de
A1 González Casado, J.M.
A1 Calvo Sorando, José Pedro
A1 Muñoz Martín, Alfonso
A1 Giner, J.
A1 Rodríguez Pascua, M.A.
AB In this paper we propose a model of tectonic and sedimentary evolution of the Spanish Central System, Toledo Mountains, Iberian - Altomira Ranges and Madrid Basin during the CenozoiCo This model hase been established from the analysis of: balanced cross sections, macro and microstructural data (analysis of brittle deformation) and the sedimentary record of Madrid Basin. These structural units, have been evolved during the Neogene, under the stress fields transmitted from the active Iberian Plate borders, the Betic and the Pyrenees. The superposition of these two regional stress tensors produces locally the «Altomira» stress field. The evolution and superposition of these regional stress fields is a gradual and long term process.
PB Seminario de Estudos Galegos. Area de Xeoloxía e Minería ;  Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
SN 0213-4497
YR 1994
FD 1994
LK https://hdl.handle.net/20.500.14352/59882
UL https://hdl.handle.net/20.500.14352/59882
LA spa
NO España. Dirección General de Investigación Científica y Técnica
DS Docta Complutense
RD 4 may 2024