Estudio de una transversal entre la cuenca de Madrid y la Cordillera Ibérica a partir de datos estructurales, sísmicos y gravimétricos.

  1. Perucha Atienza, María Ángeles
  2. Muñoz Martín, Alfonso
  3. Tejero López, Rosa María
  4. Bergamín de la Viña, Juan Francisco
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1995

Número: 18

Páginas: 15-19

Tipo: Artículo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

Resumen

An integrated geophysical and geological study has been carried out along a trasverse extending from the Madrid Basin to the Iberian Range. Geological and seismic reflection data were used as background model for the gravity modeling. Mesozoic cover structure is characterized by thrusts, E dipping, associated with a decollement located in triassic beds. Gravity modeling shows that high-angle faults bound basement blocks. The faults control triassic sediments thickness

Fuente de los datos: Dialnet