Listar REV - CLXL - Vol. 19 (1994) por título
Mostrando ítems 21-27 de 27
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Las paleoalteraciones sobre el zócalo hercínico ibérico: aproximación a una interpretación regional a partir de perfiles españoles
(Universidade da Coruña, 1994)The Hercynian basement of the Iberian Peninsula has undergone different stages of supergenic weathering which has given rise to a superposition of several «weathering mantles». Remnants ofan old weathering mantle, Mesozoic ... -
El plutón de Linares (Jaén): cartografía, petrología y geoquímica
(Universidade da Coruña, 1994)[Abstract] Magma emplacement within the Linares granite, a part of the Los Pedroches Batholith, took place in the sequence: biotite granodiorite with microgranular enclaves, biotite monzogranites, and dike swarm complexo ... -
Los problemas pendientes en la evolución morfológica del Sistema Central
(Universidade da Coruña, 1994)The Quaternary Landscape evolution in the Spanish Sistema Central range show a poor coupling with tectonic and climatic knowledge. Morphogenic activity shows more activity that could be explained in relation with accepted ... -
Reactivación alpina de pliegues y fallas del zócalo hercínico de la Cordillera Ibérica: Ejemplos de la Sierra de la Demanda y la Serranía de Cuenca
(Universidade da Coruña, 1994)[Abstract] The structure of the Variscan basement of the Iberian Chain conditioned the geometry and orientation ofstructures formed during the Alpine compression. In the Sierra de la Demanda, located in the north-western ... -
El relieve del Macizo Hespérico: génesis y cronología de los principales elementos morfológicos
(Universidade da Coruña, 1994)[Abstract] Erosion surfaces are the main geomorphological features ofthe Hesperian Massif. However, three other physiographic elements define the present state of the landscape. Such are big mountain blocks with polygonal ... -
Las rocas albíticas (albititas) del Norte de Lugo y Asturias (zona asturoccidental leonesa)
(Universidade da Coruña, 1994) -
The Pangaean inheritance
(Universidade da Coruña, 1994)[Abstract] Very old palaeosurfaces have been identified and dated in several parts of the former Gondwana and Laurasia. In Australia the separation from Antarctica was complete by the end of the Eocene so that any surface ...