RT Journal Article
T1 Estructura y metamorfismo del Macizo Hercínico de Rehamna (Meseta Occidental, Marruecos)
T1 Structure and metamorphism of the Hercynian Rehamna Massif (Western Meseta, Morocco)
A1 Aghzer, A. M.
A1 Arenas, R.
AB The structure of the Rehamna Massif, in the Moroccan Hercynian Belt, can be related to the development of a first compressive regime followed by another one of extensional character. The Skhour Nappe and Eastern Rehamna were emplaced to the W or NW during the compressive regime, simultaneously with the development of prograde metamorphism of barrovian affinity. The extensional tectonic gave rise to different ductil shear zones with contemporary retrogressive metamorphism, which caused the extension of the belt to the NE and to the 5E. The extensional regime is at the origin of the marked condensation of the barrovian metamorphic zones
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13483
UL http://hdl.handle.net/10272/13483
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026