@article{10272/8639,
year = {2006},
url = {http://hdl.handle.net/10272/8639},
abstract = {Occurrence of tectonites with features characteristic of both pseudotachylytes and ultramylonites formed
under high-pressure granulite-facies conditions is reported in the Cabo Ortegal Complex of NW Spain. We
interpret that these rocks were originated due to a seismic event at great depth (1.4 GPa) under high
temperatures (740 ºC). Shear heating would have affected the still hot and mechanically rigid granulites
and provoked melt formation. Ambient high P and T would have led to subsequent recrystallization of the
previously formed melt giving rise to a weak planar fabric},
publisher = {Sociedad Geológica de España},
title = {Ultramilonitas de apariencia fluidal, pseudotaquilitas o algo intermedio? (Formación Bacariza, Cabo Ortegal)},
title = {Ultramylonites of fluidal appearance, pseudotachylytes or something in between? (Bacariza Formation, Cabo Ortegal)},
author = {Puelles, Pablo and Ábalos, Benito and Gil Ibarguchi, José Ignacio},
}