REV - CLXL - Vol. 19 (1994): Envíos recentes
Mostrando ítems 16-20 de 27
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Dimensionamiento y sostenimiento de minas subterráneas de pizarra
(Universidade da Coruña, 1994)[Abstract] We've studied the conditions about dimensions and support ofan underground mine of roofing slate in Galice, worked by rooms with continuous pillars. The rock mass was characterized by the empiric and analitic ... -
Evolución tectonotermal asociada con extensión a escala cortical: el ejemplo hercínico del domo gneísico del Tormes (NO Salamanca, Macizo Ibérico)
(Universidade da Coruña, 1994)[Abstract] The tectonothermal Variscan evolution ofthe Tormes Gneiss Dome is controlled by a subhorizontal ductile shear zone of crustal scale and extensional characteristics, that induced a quick exhumation ofthe deep ... -
Interpretación de la estructura de la zona NE de la cuenca de Madrid mediante datos gravimétricos
(Universidade da Coruña, 1994)[Abstract] Modelling of five profiles in the NE area of Madrid Basin shows that low anomalies are related to both the thicker sediments infill of the Basin and the basement rocks like gneiss and granites. The highs are ... -
Las Cuencas Terciarias gallegas en la terminación occidental de los relieves pirenaicos
(Universidade da Coruña, 1994)[Abstract] The structure shown by the Tertiary basins ofNW Spain is in agreement with a N-s shortening. These structures are specially well exposed in As Pontes and Meirama basins which belortg to a group of basins genetically ... -
Los modelos genético-evolutivos del Sistema Central Español: implicaciones Morfotectónicas
(Universidade da Coruña, 1994)[Abstract] The characteristic morphostructure of the Spanish Central System corresponds to that of an ancient leveled massif, reactivated during the Tertiary Age by tectonic impulses related to the Alpine Orogeny; that is ...