RT Journal Article
T1 Unidades Preordovícicas y Megaestructuras Cadomienses en La Serena y La Siberia Extremeña (Macizo Ibérico meridional)
T1 Pre-Ordovician units and Cadomian megastructures of La Serena and La Siberia Extremeña(Southern Iberian Massif)
A1 Apalategui, Octavio
A1 Eguiluz, Luis
A1 Martínez Torres, Luis M.
A1 Palacios Medrano, Teodoro
AB 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 thedistinction of up to four independent stratigraphic units. The studied sequence is exposed in twomegastructures: the Almorchón-Valdecaballeros Antiform and the Cerro de los Moros Synform, separatedby the Patin Fault, which seems to correspond to an ancient paleogeographic boundary. The continuity ofthese structures under the Paleozoic synclines and the sub-orthogonal directions with respect to those ofthe 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
YR 2009
FD 2009
LK http://hdl.handle.net/10272/7999
UL http://hdl.handle.net/10272/7999
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026