RT Journal Article
T1 Ultramilonitas de apariencia fluidal, pseudotaquilitas o algo intermedio? (Formación Bacariza, Cabo Ortegal)
T1 Ultramylonites of fluidal appearance, pseudotachylytes or something in between? (Bacariza Formation, Cabo Ortegal)
A1 Puelles, Pablo
A1 Ábalos, Benito
A1 Gil Ibarguchi, José Ignacio
AB Occurrence of tectonites with features characteristic of both pseudotachylytes and ultramylonites formedunder high-pressure granulite-facies conditions is reported in the Cabo Ortegal Complex of NW Spain. Weinterpret that these rocks were originated due to a seismic event at great depth (1.4 GPa) under hightemperatures (740 ºC). Shear heating would have affected the still hot and mechanically rigid granulitesand provoked melt formation. Ambient high P and T would have led to subsequent recrystallization of thepreviously formed melt giving rise to a weak planar fabric
PB Sociedad Geológica de España
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8639
UL http://hdl.handle.net/10272/8639
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026