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- W55961215 abstract "A study dealing with quartz microstructures and -C- axis fabrics within mylonite-series rocks from the Badajoz-Cordoba Ductile Shear Belt (SW Iberian Massif) is presented. Deformation regimes, geometries, temperatures, and kinematics are determined, as well as deformation histories responsible for the development of crystallographic preferred orientations (pan-african and variscan orogenic episodes). The geometry of variscan deformation (alternating areas with upright and horizontal mylonitic foliations containing ultramylonitic corridors) and mechanisms (complex deformation regimes characterized by the presence of neighbouring rock volumes affected by heterogeneous simple shear, flattening, heterogeneous simple shear plus flattening, buckling followed by flattening, etc.) are discussed from the perspective of deformation dynamics within ductile shear zones. Variscan, transcurrent, left-Iateral, tectonic displacements in the Badajoz-Cordoba Ductile Shear Belt have been estimated at ca. 200-300 km. Their regional implications in relation to the variscan emplacement of Allochthonous Complexes from NW Spain are discussed." @default.
- W55961215 created "2016-06-24" @default.
- W55961215 creator A5033914725 @default.
- W55961215 creator A5066047621 @default.
- W55961215 date "1990-08-30" @default.
- W55961215 modified "2023-10-02" @default.
- W55961215 doi "https://doi.org/10.3989/egeol.90463-4451" @default.
- W55961215 hasPublicationYear "1990" @default.
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