@article{10272/13432,
year = {1995},
url = {http://hdl.handle.net/10272/13432},
abstract = {The final stages of late-Hercynian granitoid plutonism in eastern Credos are represented by a series of small issolated peraluminous plutons belonging to the same evolutionary trend than the previous granitic complexes. They are biotite ±muscovite-bearing monzogranites and leucogranites in continuity with the differentiation process that gave rise to this hugh granitic province, mainly controlled by fractional crystallization of plagioclase, K-feldspar and minor amounts of biotite and zircon},
publisher = {Sociedad Geológica de España},
title = {Plutonismo peralumínico tardihercínico en el sector oriental de Credos (Sistema Central Español): Caracterización y relación con etapas previas},
title = {Late-Hercynian peraluminous plutonism in eastern Credos (Spanish Central System): Characterization and relationship with previous stages},
author = {Herreros Villanueva, V. M.},
}