RT Journal Article
T1 Metapelitas de alta presión de la Unidad de Santiago (Complejo de Ordenes, NO del Macizo Ibérico)
T1 High - pressure metapelites from the Santiago Unit (Ordenes Complex, NW of the Iberian Massif)
A1 Rubio Pascual, F. J.
A1 Arenas, R.
A1 Díaz García, F.
AB A high - pressure - low - to intermediate temperature eo - Hercynian metamorphic event characterizes the tectonothermal evolution of the Santiago Unit, in the western margin of the Ordenes Complex. P-T conditions fo r the mineral assemblages of the high - pressure event (which is essentially preserved as a very thin Si=S1 included in albite porphyroblasts in semipelitic schists) have been estimated at 493 ± 9 °C and 14.7 ± 0.7 kbar (minimum pressure). The development of the high - pressure metamorphism and the lacking of significative reequilibrium of their characteristic mineralogy, suggests that the unit (probably a fragment o f the continental margin of Condwana) has been uplifted inm ediately after undergoing subduction in the beginning of the Hercynian Orogeny
PB Sociedad Geológica de España
YR 1992
FD 1992
LK http://hdl.handle.net/10272/14137
UL http://hdl.handle.net/10272/14137
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026