Barita de neoformación en la Arenisca de Villamayor (Salamanca)estudio preliminar
- Alonso-Gavilán, G. 1
- Moro, M.C. 1
- Cembranos, M.L. 1
- Areas, A. 2
- 1 Universidad de Salamanca, España
- 2 Minas y Geología. Salamanca, España
ISSN: 0213-683X
Año de publicación: 1997
Título del ejemplar: 22ª Sesión Científica, Bilbao 1997
Número: 22
Páginas: 15-17
Tipo: Artículo
Otras publicaciones en: Geogaceta
Resumen
The barite studied in the Villamayor sandstone is located in old rhizoliths related to subvertical fractures which affect these subarcosic deposits. These zones are actually in great circulation within underground waters and fuIl of clay materials. The mineral' s form together with ist mineralogical, chemical and isotopic characteristics suggests that its formation is related with the postneogene alteration processes (caolinitization) of sandstones which libera te Ba of the feldspars and with the infiltration and circulation of metheoric waters that contain dissolved sulphates.