@article{10272/8249,
year = {2008},
url = {http://hdl.handle.net/10272/8249},
abstract = {The initial growth stage of the Fuerteventura Island is represented by submarine, transitional and subaerial
volcanics. Among the submarine types, two can be distinguished: a basaltic (s.l.) one, and a basanitic one.
The latter is characterized by the presence of hydrous ferromagnesian minerals (kaersutite, phlogopite)
and a more alkaline character, whereas the former shows a less alkaline character that brings it closer to
the subaerial group. All these groups would be generated from different partial melt degrees of a garnetbearing
mantle source. However, for the basanitic group, also a shallower (oceanic lithosphere) melting
and an amphibole-bearing source have to be invoked},
keywords = {Submarine-subaerial},
keywords = {Basaltic-basanitic volcanism},
keywords = {Mineralogy},
keywords = {Geochemistry},
keywords = {Fuerteventura},
title = {Diferencias mineralógicas y geoquímicas del vulcanismo inicial de Fuerteventura},
title = {Mineralogical and geochemical differences of the initial volcanism of Fuerteventura},
author = {Muñoz, Mercedes and Sagredo, J. and Ignacio, Cristina de},
}