ARQ - Série Ciências da Natureza
Permanent URI for this community
Browse
Browsing ARQ - Série Ciências da Natureza by Subject "Água de Pau"
Now showing 1 - 2 of 2
Results Per Page
Sort Options
- Petrogenesis of the recent trachytic pyroclastic succession of Agua de Pau Volcano, (Sao Miguel, Azores)Publication . Storey, MichaelThe recent stratigraphy of São Miguel records large numbers of trachytic pyroclastic deposits produced by plinian to sub-plinian eruptions. Tephrochronological studies by Booth, Croasdale and Walker (1978) have shown that in the last five thousand years there have been five such eruptions from Agua de Pau, one of three active stratovolcanoes on São Miguel. A geochemical and electron microprobe study made on the resultant pyroclastic succession, revealed significant variations in pumice clast chemistry and mineralogy between the individual deposits. For example, Sr and Eu/Eu* decrease in value through the succession, whereas 'incompatible' elements such as La, Zr and Nb show stepwise enrichment attaining highest concentrations in the most recent deposit. The individual pyroclastic deposits are interpreted as representing successive samp1es of a body of trachyte magma undergoing appreciable crystal fractionation. However not ali of the observed chemical and mineralogical variations of the pyroclastic deposits are consistent with simple differentiation. For example, evidence is presented that trachyte magma has periodically mixed with intermediate and basaltic magmas. Magma mixing has found to be a recurrent feature of many of the lavas and pyroclastic deposits from Agua de Pau. Associated lavas possessing REE patterns with positive Eu anomalies and mineralogical peculiarities are also discussed. A case is made for the existence of a compositionally zoned magma chamber beneath Agua de Pau volcano.
- The petrology and geochemistry of the Água de Pau Volcano, São Miguel, AzoresPublication . Marriner, Giselle Frances; Norry, M. J.; Gibson, I. L.During recent years several geochemical investigations have centred upon the Azores (Schmincke 1973, Schmincke and Weibel 1973, Flower et al., 1976, White et al., 1979) with particular emphasis being laid upon inter island differences. Islands have been characterised as being relatively potassic (São Miguel) less potassic (Flores and Santa Maria) and sodic (Pico, Fayal, São Jorge, Graciosa and Terceira) (Flower et al., 1976). However, several of these islands are complex, consisting of several centres displaying multiple compositional trends. In this study we have concentrated upon lavas erupted from one volcano, that of Agua de Pau on the island of São Miguel. The volcano consists of a central cone from whose caldera explosive trachytic eruptions have taken place. Basic and intermediate subsidiary cones are situated on its flanks, which have produced both lava flows and pyroclastics (Booth et al., 1978).