@article{10272/10237,
year = {1997},
url = {http://hdl.handle.net/10272/10237},
abstract = {The marginal zones of the Maestrazgo Basin (Las Parras and Galve basins) and the Algarve Basin show a similar evolution during basin formation (mainly Jurassic and Early Cretaceous) and inversion (Oligocene-Early Miocene). Common features between the two basins are the control of sedimentation during extension by basement normal and transfer faults (NW-SE and NE-SW) and the complete inversion during the Tertiary accomodated by basement-involved E-W thrusts, preserving the extensional geometry with non-reactivated normal faults at the thrusts hanging-walls. Extensional structures in the Las Parras and Calve basins are consistent with a roughly N-S oriented extension (locally NE-SW and NW-SE, perpendicular to the main normal faults). Thrusts show an overall E-W direction compatible with a near N-S shortening between the Late Eocene and the Early Miocene. Extension in the Algarve Basin was accomodated by ENE-WSW to NE-SW late Variscan faults; NW-SE transfer faults dipping to the Northeast also accomodated some extension and divided the area into sub-basins. Inversion in the Algarve Basin pre-dated deposition ofthe Miocene sediments and was accomodated by S- to S-SE directed thrusts, which cross-cut the main extensional faults},
publisher = {Sociedad Geológica de España},
keywords = {Sedimentary basin},
keywords = {Basin inversion},
keywords = {Basement fault},
keywords = {Mesozoic},
keywords = {Tertiary},
keywords = {Iberian plate},
title = {Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica},
title = {Comparative study ofthe evolution and inversión ofseveral Mesozoic basins within thè Iberian píate},
author = {Casas Sainz, Antonio and Cortés Gracia, A. L. and Liesa, Carlos L. and Soria, Ana Rosa and Terrinha, P. and Kullberg, J. C. and Rocha, R. da},
}