@article{10272/8808,
year = {2004},
url = {http://hdl.handle.net/10272/8808},
abstract = {We describe the main features of the Campillo shear zone, a band of intense deformation made of mylonitic
to ultramylonitic rocks bearing a vertical foliation and subhorizontal stretching lineations. The shear zone
is more than 2 km thick and extends along more than 100 km representing one of the largest tectonic
structures of the Ossa-Morena Zone, comparable to the Badajoz-Córdoba Blastomylonitic Belt. Its longlasting
activity and influence on the paleogeography and stratigraphy of a number of sedimentary sequences
allow to consider the Campillo shear zone as an exceptional example of a continental-scale rectilinear
high-angle fault zone within the Variscan orogen},
publisher = {Sociedad Geológica de España},
title = {La zona de cizalla de Campillo: accidente tectónico a escala continental en el suroeste del Macizo Ibérico},
title = {Campillo shear zone: continental tectonic structure in the southweast of the Iberian Massif},
author = {Eguiluz, Luis and Apalategui, Octavio and Carracedo Sánchez, Manuel and Sarrionandia Eguidazu, Fernando},
}