@article{10272/14123,
year = {1992},
url = {http://hdl.handle.net/10272/14123},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Evolución tectonotermal de la Unidad de Santiago (Complejo de Ordenes): un ejemplo de subducción eo-hercín¡ca y descompresión sin-colisional},
title = {Tectonothermal evolution of the Santiago Unit (Ordenes Complex): an example of eo-Hercynian subduction and syn-collisional decompression},
author = {Rubio Pascual, F. J. and Arenas, R. and Díaz García, F.},
}