@article{10272/8359,
year = {2007},
url = {http://hdl.handle.net/10272/8359},
abstract = {Metapelitic schists from the upper structural levels of the Malpica-Tui Unit contain an initial blueschist
facies mineral assemblage that appears mainly preserved as micro-inclusions in garnet, albite and chloritoid
porphiroblasts defining a S1 foliation. The main foliation (S2) represents an evolution of the S1 to slightly
higher temperature and lower pressure, but it is still developed in blueschist facies conditions. Post-S2
deformations include restricted development of spaced C’ shear bands, tight and straight D3 folds and a
later gentle subhorizontal crenulation formed in greenschists facies conditions. Garnet-phengite thermometry
and GRIPS and GASP barometry calculations, using micro-inclusion compositions, indicate peak conditions
around P=19-22 Kbar and T=430-500 ºC. The same calculations using the S2 fabric minerals yield
approximate values of P=16-19 Kbar and T=440-515 ºC},
title = {Evolución metamórfica de los esquistos de AP/BT de Ceán (Unidad de Malpica-Tui, NW del Macizo Ibérico)},
title = {Metamorphic evolution of the HP/LT Ceán schists (Malpica-Tui Unit, NW Iberian Massif)},
author = {López Carmona, A. and Abati, Jacobo and Reche, J.},
}