RT Journal Article
T1 Evolución tectonotermal de la Unidad de Santiago (Complejo de Ordenes): un ejemplo de subducción eo-hercín¡ca y descompresión sin-colisional
T1 Tectonothermal evolution of the Santiago Unit (Ordenes Complex): an example of eo-Hercynian subduction and syn-collisional decompression
A1 Rubio Pascual, F. J.
A1 Arenas, R.
A1 Díaz García, F.
AB The syn-D2 uplift of the Santiago Unit, inmediately after of the high-pressure eo-Hercynian metamorphic event, cause a markedly decompressive-slightly prograde P,T,t path. This path very likely suggests that the majority of the rising history of the unit took place in a context of ductile extension, related to the continued underplating of the continental margin of Condwana and compensating extension above. The actual disposition of the syn-D2 metamorphic zones is inverse, w ith the staurolite zone (which represents the thermal peak) occupying the top o f the unit
PB Sociedad Geológica de España
YR 1992
FD 1992
LK http://hdl.handle.net/10272/14123
UL http://hdl.handle.net/10272/14123
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026