Listar REV - CLXL - Vol. 22 (1997) por data de publicación
Mostrando ítems 1-13 de 13
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Análisis tafonómico de la muestra ósea de Liñares sur (Lugo, Galicia)
(Universidade da Coruña, 1997)[Abstract] This paper deal with the biostratinomic processes and fossildiagenetic processes which affected the bone rest of Pleistocene age from the Liñares Sur carstic cave. AH show that the active processes was creepy ... -
Compacidad de los suelos desarrollados sobre sedimentos Terciario-Cuaternarios en Terra Cha (Lugo)
(Universidade da Coruña, 1997)[Abstract] Using a gamma probe, bulk density has been measured for nine profiles from 20 cm depth to depths ranging from 90 to 15Ocm. The intent ofthis work was to assesss total porosity variability withinand between sites ... -
Relación entre textura, pH, materia orgánica y complejo de cambio en el horizonte superior de un suelo sobre serpentinas
(Universidade da Coruña, 1997)[Abstract] A statistical analysis of texture, pH, organic matter content and CEC in the rop horizon of a soil over serpentine underneath was undertakan. The studied properties showed a considerable variability. Significant ... -
Géomorphologue granitique du Massif de l'Andringitra: Sa relation avec l'évolution de l'Île pendant le Cénozoïque
(Universidade da Coruña, 1997)[Abstract] The Andringirra Massif is a srratoide granite on the south of the Isle of Madagascar. Is a residual reliefwhich represents one ofthe last remnants of the Gondwana surface at the island egraded after the break ... -
Evolución postglaciar de la laguna de Villaseca (NW de la Península Ibérica) a partir del análisis de diatomeas
(Universidade da Coruña, 1997)[Abstract] The lake of Villaseca is located in the foothills of the southern Cantabrian Mountains, nearby Villaseca de Laciana (León,NWIberian Peninsula). This lake has a glacier origin and has been formed due to the ... -
Evolución neógena de la cuenca baja del Tambre
(Universidade da Coruña, 1997)[Abstract] The present paper srudy the evolution of the lower part of the Tambre Basin duting the Neogene. The basin, the fluvial network and a group of features are analyzed, such as the asymmetry of the net, the ... -
Geomorphology of the Bushveld Complex
(Universidade da Coruña, 1997)[Abstract] This paper deals wich che differenc relacion becween scruccure and lichology in che geomorphology of che Bushveld Complexo The final resules demonscrace chac, even so differenc scale ofsize, wider for che ... -
Condicionantes en la distribución de macromamíferos en Galicia (NW Península Ibérica) durante el Cuaternario superior
(Universidade da Coruña, 1997)[Abstract] Galicia, in theNWofthe Iberian Peninsula, was a transit area for the migrating large mammals during the Upper Quaternary. These migrations were praduced by the c1imatic changes that characterize this periodo A ... -
Variables de control en la génesis y desarrollo del modelado granítico: análisis de microformas en el macizo de Manzaneda (Galicia, España)
(Universidade da Coruña, 1997)[Abstract] Morphometric analysis results from Manzaneda granitic massif(Galicia, Spain) is displayed. Field observations ofgnammas sample are subject to exploratory and multivariate techniques. Explanation results provide ... -
Relación entre las intrusiones plutónicas y el complejo filoniano en el batolito de Los Pedroches (Macizo Ibérico, España): los diques como indicadores de ambientes paleotectónicos y paleoesfuerzos
(Universidade da Coruña, 1997)[Abstract] The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large biotite ±amphibole granodiorite pluton and several, smaller variable porphyritic, biotite ± cordierite granite intrusions. A dyke ... -
La extremidad occidental de la superficie fundamental de Galicia: La Meseta de Santa Comba
(Universidade da Coruña, 1997)[Abstract] The Plateau ofSanta ir Comba is a very degraded rest ofan old surface (Late-Mesozoic -Paleogene), ofcomplex history. It has a mean altitude of400 m, and it is located in the western part of the Coruñan province. ... -
Models of landscape evolution and the survival of Palaeoforms
(Universidade da Coruña, 1997)[Abstract] Qne ofthe factots rnitigating against the recognition and acceptance ofvery old palaeosurfaces was, and in sorne rneasure rernains, the tacit acceptance ofsorne ofthe better known rnodels oflandscape evolution. ... -
Contribución al conocimiento de la vegetación holocena en el NO de la Península Ibérica (Galicia, España)
(Universidade da Coruña, 1997)[Abstract] A paleobocanic scudy ofcwo Galician sierras, Coure! siecra and Queixa-Invernadoiro sierra is presenced here. A palynological scudy ofche Laguna Lucenza was carried ouC in che Coure! sierra. Eighc radiocarbon ...
