Thesis Collection
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Browsing by Author "Galindo, Carmen"
Now showing items 21-26 of 26
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Geocronologia Rb-Sr de los leucogranitos del complejo plutonico de Burguìllos del Cerro (Badajoz)
(Sociedad Geológica de España, 1996)A Rb-Sr whole-rock array corresponding to an age of circa 330M. a. has been obtained for the slightly to moderately peraluminous leucogranites of the Burguillos del Cerro Massif. The samples were collected from several ... -
Granitoides peraluminosos y su relación con las rocas fuentes
(Sociedad Geológica de España, 2005)Comparative compositional studies between two peraluminous unit with magmatic andalucite and cordierite indicate that they were produced by partial melting of two differents metasedimentary source rocks. We conclude that ... -
La evolución isotópica de los fluidos ligados a los Sistemas Hidrotermales tardi y postvariscos del Sistema Central Español
(Sociedad Geológica de España, 1996)The late to postvariscan hydrothermal activity of the Spanish Central System extends almost from ca. 300 Ma to the present. It consists of several Independent stages that can be grouped in two different hydrothermal regimes. ... -
Las cloritas de los cuerpos pegmatíticos del plutón de La Cabrera (Sistema Central Español)
(Sociedad Geológica de España, 1996)The chlorites included within the pegmatitic bodies of the La Cabrera pluton (Spanish Central System) have been studied in order to stablish their characterization, clasification and relationship with other minerals. Two ... -
Las mineralizaciones ferríferas del coto minero San Guillermo (Jerez de los Caballeros, Badajoz, España)
(Sociedad Geológica de España, 2005)Stratoid magnetite and skarn magnetite were mined at the San Guillermo mine district. Structural and textural evidence suggest that they formed by replacement of older rocks in Variscan orogeny times during a protracted process ... -
El metamorfismo en la Cuenca de los Cameros. Geocronología e implicaciones tectónicas
(Sociedad Geológica de España, 1991)A case of hydrothermal metamorphism is described from the Cameros Basin along the rio Cidacos transect. The highest grade is reached at the base of the Urbión Group, a fluvial sequence Upper Jurassic to Lower Cretaceous ...
