%0 Journal Article
%T Petrology of the Volcanic Rocks from Bioko Island (¡°Cameroon Hot Line¡±)
%A Fadimatou Ngounouno Yamgouot
%A Bernard D¨¦ruelle
%A Isaac Bertrand Gambie Mbowou
%A Isma£¿la Ngounouno
%J International Journal of Geosciences
%P 247-255
%@ 2156-8367
%D 2015
%I Scientific Research Publishing
%R 10.4236/ijg.2015.63019
%X Bioko island (3008 m
a.s.l.), is composed of the alkaline basaltic lavas (basalts and hawaiites)
with xenoliths. These lavas have a microlitic textureand consisted of euhedral
to subhedral phenocrysts (>1
mm) of olivine (0.83 < Mg# < 0.87) and diopside ¡À Ti-augite. Plagioclase
(An62-67Ab35-32Or3-1) phenocrysts are present
only in hawaiites. In Harker diagrams, SiO2, Al2O3,
Na2O and K2O contents of the lavas increase and Fe2O3,
MgO and CaO decrease with increasing differentiation from basalts to hawaiites.
The compatible elements Ni, Cr and V decrease strongly in basalts and remain at
low levels in hawaiites. Basaltic lavas from Bioko lavas have low Hf contents
(4.2 - 9.2 ppm) and consequently higher Hf/Zr ratios (50 - 90) than those
(<50) of similar lavas from other volcanoes of the Cameroon Hot Line. Such
high ratios are commonly observed in alkaline basaltic lavas associated with
carbonatitic and/or nephelinitic magmatism. The Sr and Nd isotopic compositions
point to a slightly depleted mantle source.
%K Petrology
%K Geochemistry
%K Lavas
%K Bioko
%K Cameroon Hot Line
%U http://www.scirp.org/journal/PaperInformation.aspx?PaperID=54987