RT Journal Article
T1 Estructuras extensionales tardías en la granodiorita de Veiga (Arco Hercínico de Galicia)
T1 Late extensional structures in the Veiga granodiorite (Hercynian Are, NW Spairt)
A1 Román Berdiel, Teresa
A1 Casas Sainz, Antonio
A1 Pueyo Morer, Emilio L.
AB At the western border of the Veiga granodiorite (Hercynian Arc of Galicia), C-S structures coexist with brittle mesostructures (faults and dykes corresponding to the late stages of emplacement). C and S structures indicate that the cooling of magma was coeval with the Chandoiro fault, a N-S striking normal fault with a N280E hanging wall displacement direction. Brittle structures were analysed by means of the Right Dihedra, Right Trihedra and Etchecopar's methods. They are consistent with a NW-SE extension direction and à vertical c, axis. The coincidence between the two extension directions means that the stress regime under which the granitoid Intruded maintained during the post-cooling stage
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10553
UL http://hdl.handle.net/10272/10553
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026