Silva, P. G.Goy, José L.Zazo, C.2019-05-292019-05-291992http://hdl.handle.net/10272/16323The Lorca-Alhama fault is one of the more tectonic and seismically active sinistraI strike-slip fault of the eastern Betics. Its complex structural pattern records simultaneous development of ex- tensional and contractional features, which can be explained by a simple sinistral shear model. Spatial coincidence of structural and geometric diagnostic features of segment boundaries along the strike of the fault, are reflecting the segmented nature of this tectonic accidentspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Structural patternGeometrySimple shearFault segmentationLorca-Alhama faultEastern Beticsjournal articleopen access