Browsing Geogaceta -- Nº 14, (1993) by Title
Now showing items 41-47 of 47
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Rasgos generales del relieve en el sector suroriental de la Sierra Almijara (Málaga)
(Sociedad Geológica de España, 1993)The morphostructural landform o f this Betics coastal sector is conditioned by lithological, structural (Neotectonics) and geomorphologicai features. Tortonian planated relief was faulting during Mio-Pliocene age by a NW-SE ... -
Relaciones entre la diagénesis orgánica y mineral en rocas madre de cuencas lacustres: cuenca terciaria de Ribesalbes
(Sociedad Geológica de España, 1993)Lacustrine carbonate sediments from the Tertiary Basin of Ribesalbes (Castellón, Spain) were studied with the aim of determining the relationships between organic and mineral diagenesis. Petrological and geochemical data ... -
Sedimentologia del sector occidental del abanico costerò de Sant Llorenf del Munt (Eoceno, cuenca de antepais surpirenaica)
(Sociedad Geológica de España, 1993)The Bartonian-Priabonian Sant Lloreng del Munt fan-delta complex is located at the SE margin of the South-Pyrenean foreland basin. During the deposition of this complex the basin margin was controlled by a series of sinistral ... -
El sistema NW-SE de fosas de Rosas y Bagur (margen continental nororiental de España)
(Sociedad Geológica de España, 1993)An analysis ofmultichanell seismic profiles leads to define the main fracture zones in the northeastern continental margin of Spain. Two fault systems have been mapped: I) NE-SW to N-S that defines a classical extensional ... -
Sobre la hidroquímica de la cuenca del río Almanzora (Almería)
(Sociedad Geológica de España, 1993)The waters of the Almanzora basin have very different chemistry according to the hydrogeological context; the mineralization is between 0,4 and more than 6 g/i; the hydrochemical facies is usually . calcic, bicarbonated ... -
El Terciario de la unidad de Saaden ("Dorsal" externa, Rif Septentrional, Marruecos)
(Sociedad Geológica de España, 1993)In the Saaden unit (External "Limestone Chain", northern Internal Rif), the uppermost Eocene and the Oligocene have been dated by planktonic foraminifera. It confirms that an important transgression accounted during the ... -
La zona de transición agua dulce-salmuera bajo el borde norte de la laguna salada de Fuente de Piedra (Málaga)
(Sociedad Geológica de España, 1993)The results of temperature and electrical conductivit y logs carrie dout in some recently drilled boreholes across the northern shoreline of the Fuente de Pledra Salt Lake, provid e the first data a bout a relative lythick ...