RT Journal Article
T1 Plutonismo peralumínico tardihercínico en el sector oriental de Credos (Sistema Central Español): Caracterización y relación con etapas previas
T1 Late-Hercynian peraluminous plutonism in eastern Credos (Spanish Central System): Characterization and relationship with previous stages
A1 Herreros Villanueva, V. M.
AB 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
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13432
UL http://hdl.handle.net/10272/13432
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 13 jul 2026