@article{10272/8578,
year = {2006},
url = {http://hdl.handle.net/10272/8578},
abstract = {In the West Asturian-Leonese Zone there are some albititic beds of volcanoclastic origin interlayered in the
lower part of the Serie de los Cabos, deposited in a graben-type basin during the Middle Cambrian. The
mineralogy is plagioclase (albite), rutile, sheet silicates and sometimes quartz, carbonates and chloriteserpentine
cryptocrystalline masses.
Melting experiments at 850ºC, 6 kbar and added 10% water conditions produce very silicic melts, with
different rates of melting according to quartz percentage, but the fertility of these rocks as sources of
leucogranites is very low},
keywords = {Albitite},
keywords = {Paredes},
keywords = {Cineritic deposit},
keywords = {Silicic melts},
title = {Las albititas del Paleozoico Inferior del occidente de Asturias: ¿posible fuente de leucogranitos?},
title = {The Lower Palaeozoic albitites from Western Asturias: possible source of leucogranites?},
author = {García Arias, M. and Corretgé Castañón, Luis Guillermo and Castro Dorado, Antonio},
}