RT Journal Article
T1 Diques de lamproítas a lo largo de la Falla de Socovos (Béticas orientales)
T1 Lamproite dikes along the Socovos Fault (Eastern Betics)
A1 Pérez Valera, Luis Alfonso
A1 Pérez Valera, Fernando
A1 Sánchez Gómez, Mario
A1 Fernández Soler, José Manuel
A1 Azor, A.
AB The Calasparra segment of the Socovos Fault shows a large number of lamproite outcrops, most of them being dikes emplaced along tension gashes and Riedel faults. Subsequently to the emplacement, some of the dikes were affected by faulting, showing striae and kinematic indicators of right-lateral displacement. The ubiquity of the lamproite outcrops, together with the mantle source invoked for these magmas, imply that the Socovos Fault is a major fracture zone, cutting through the crust and connecting in some way the surface to the lithospheric mantle
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7856
UL http://hdl.handle.net/10272/7856
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026