Zobrazeno 1 - 10
of 14
pro vyhledávání: '"J R Vidal Romaní"'
Autor:
J. Yepes Temiño, J. R. Vidal Romaní
Publikováno v:
Estudios Geologicos, Vol 60, Iss 1-2, Pp 21-35 (2004)
El presente trabajo ofrece un análisis preliminar de la red fluvial con antecedencia terciaría del sureste gallego. Las observaciones geomorfológicas de campo se centran en la cartografía de terrazas erosivas, canales abandonados, meandros colgad
Externí odkaz:
https://doaj.org/article/9188afa45b6c4981ac95459be0f1d2f9
Autor:
J. Yepes Temiño, J. R. Vidal Romaní
Publikováno v:
Estudios Geologicos, Vol 58, Iss 5-6, Pp 179-188 (2002)
Se presenta el análisis morfológico de un sector del replano Rlooo. El sector escogido está colgado por encima de la red fluvial actual. Este hecho permite atribuir a los cursos que drenan el replano un carácter semi funcional. Se han identificad
Externí odkaz:
https://doaj.org/article/734c7b967be44d4b90e8b70a095654b9
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
The Centro de Investigação Geológica, Ordenamento e Valorização de Recursos is supported by the Pluriannual program of the Fundação para a Cência e a Tecnologia, funded by the national budget of the Portuguese Republic.
Deposition of gas
Deposition of gas
Publikováno v:
Water, Air, and Soil Pollution. 204:53-68
Gypsum-rich coatings found on buildings constructed with granitic rock ashlars have been studied, from both an urban and a rural area of the NW of Spain. Previous works have attributed gypsum to rock weathering by atmospheric pollution. Mineralogical
Publikováno v:
X-Ray Spectrometry. 37:346-354
The Casas de Paredes (A Coruna, Spain) is an example of 18th Century neoclassical architecture built with˜granitic rocks. There are neoformation coatings on the main fa¸cade of one of the buildings, producing avisible soiling. Sixteensamplesof coat
Publikováno v:
Quaternary International. :45-51
Two cores from Andringitra Massif (Madagascar), the peatbog of Andonaham Pasipotsy (2000 m a.s.l.) and Amboromena Lac (2400 m a.s.l.), have been analysed to reconstruct the late Pleistocene–Holocene (last 12,000 yr BP) evolution of the area. Andona
Publikováno v:
Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms. 172:832-837
Late Pleistocene glaciations in the NW Iberian Peninsula over Serra de Queixa and Serra de Xures, all with granite substrata, were studied by mass spectrometry using cosmogenic 21Ne. Rock cores were drilled in glacial polished surfaces and push-morai