@article{10272/10323,
year = {1997},
url = {http://hdl.handle.net/10272/10323},
abstract = {Detailed structural, interpretátioh of a network of high-resolution seismic lines runnig across, , and along the continental shelf of Faro (south-lberian Atlantic margin) provides evidences of recent deformation structures associated with the Africa-Eurasia plate boundary. In these seismic profiles, palm-tree type flower structures interpreted as strike-slip faults affect the non-consolidated Holocene muddy shelf deposits and the underlying semi-cemented sandy shelf-wedges of the Pleistocene units. These structures are lined up following a ENE-WSW. direction, associated with the existence of a deeper dextral transcurrent basement fault with recent active seismicity between the southern Coringe Bank, Horseshoe Plain, Faro continental shelf and northern of Guadalquivir basin},
publisher = {Sociedad Geológica de España},
title = {Neotectómca transpresiva en la plataforma continental Suribérica Atlántica},
title = {Transpresive neotectonics along South-lberián Atlantic shelf},
author = {Maestro González, Adolfo and Somoza, L. and Díaz del Río, Víctor and Vázquez Garrido, Juan Tomás and Martín Alfageme, S. and Alveirinho, J. M. and Barnolas, Antonio and Vegas, Ramón},
}