2026-06-28T04:48:20Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/598822024-08-02T13:43:38Zcom_20.500.14352_14col_20.500.14352_15

Evolución y estructuras alpinas en la zona del centro peninsular Vicente Muñoz, Gerardo De González Casado, J.M. Calvo Sorando, José Pedro Muñoz Martín, Alfonso Giner Robles, Jorge Luis Rodríguez Pascua, M.A. 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. 2023-06-20T20:13:29Z 2023-06-20T20:13:29Z 1994 journal article 0213-4497 https://hdl.handle.net/20.500.14352/59882 http://www.iux.es/?page=5&serie=1 spa PB91-0397 open access Seminario de Estudos Galegos. Area de Xeoloxía e Minería ; Instituto Universitario de Xeoloxía "Isidro Parga Pondal"