RT Journal Article
T1 Características de la red de diques graníticos intruidos en las peridotitas de Ronda (Cordilleras Béticas)
T1 Characterization of the granite dyke swarm within the Ronda peridotites (Betic Cordilleras)
A1 Esteban, José Julián
A1 Cuevas, Julia
AB This work analyses, from the structural point of view, the granite dyke swarm in the R onda area. Structuralfeatures of granite dykes from outcrop to microscopic scale show that their intrusion is controlled by theemplacement of the peridotites over the underlying crustal rocks and prove that granite dyke swarm is notplaced randomly. Actually, the orientation of deformed and undeformed dykes provides an indirect butuseful tool to determine the kinematic criteria of the hot emplacement of the Ronda peridotites, especiallyin areas where the ultrabasic rocks are extremely sepentinized. Finally, we also discuss the origin of thegranite magma concluding that the continental crust is the most likely source
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8450
UL http://hdl.handle.net/10272/8450
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026