@article{10272/7999,
year = {2009},
url = {http://hdl.handle.net/10272/7999},
abstract = {New mapping of the pre-Ordovician basement (Schist and Greywacke Complex or Lower Alcudian)
from the La Serena and La Siberia Extremeña regions of the southern Central Iberian zone has allowed the
distinction of up to four independent stratigraphic units. The studied sequence is exposed in two
megastructures: the Almorchón-Valdecaballeros Antiform and the Cerro de los Moros Synform, separated
by the Patin Fault, which seems to correspond to an ancient paleogeographic boundary. The continuity of
these structures under the Paleozoic synclines and the sub-orthogonal directions with respect to those of
the Variscan cover is regarded as an evidence for deformational events related to the Cadomian (pan-
African) cycle, likely in connection to those recorded in the adjacent Ossa-Morena Zone},
title = {Unidades Preordovícicas y Megaestructuras Cadomienses en La Serena y La Siberia Extremeña (Macizo Ibérico meridional)},
title = {Pre-Ordovician units and Cadomian megastructures of La Serena and La Siberia Extremeña
(Southern Iberian Massif)},
author = {Apalategui, Octavio and Eguiluz, Luis and Martínez Torres, Luis M. and Palacios Medrano, Teodoro},
}