@article{10272/18344,
year = {1989},
url = {http://hdl.handle.net/10272/18344},
abstract = {Se han determinado las relaciones isotópicas de oxígeno de varios tipos de granitos y migmatitas (nebulitas cordieríticas) en sectores occidentales del Macizo Central español. Granitos biotíticos y biotítico-anfibólicos muestran valores de ð18O entre 9 y 10,50/00 (SMOW). Las nebulitas muestran una mayor variación (10-130/00). Los granitos con cordierita tienen valores intermedios (entre 9,8 y 10,50/00), sugiriendo la posibilidad de ser el resultado de la asimilación de nebulitas por el magma que origina los granitos biotíticos},
abstract = {The relationships of oxygen isotopic of various types of granites and migmatites (cordierite nebulite) in western regions of the Central Iberian Massif, Spain, have been determined. Biotites and biotite-amphibolites show values of ð18O between 9 and 10,50/00 (SMOW). The nebulites show a greater variation (10-130/00). The granites with cordierite have intermediate values (between 9,8 and 10,50/00), which suggest the possibility of being the result of the assimilation of the nebulites by the magna which cause the biotite-granites.},
publisher = {Sociedad Geológica de España},
title = {ô 180 of granites from the Western Central Iberian Massif, Spain},
author = {Ugidos, José María and Fallick, A. E. and Recio, Clemente},
}