@article{10272/9586,
year = {2001},
url = {http://hdl.handle.net/10272/9586},
abstract = {The Ribadelago and Sotillo plutons are located in the Central Iberian Zone, a tectonic domain of the Iberian Variscan belt (NW Spain). These synkinematic granitoids are composed by swarms of sheeted intrusions parallel to the overall elongation, 130°E, of both plutons. Most of these igneous sheets show pronounced planar fabrics and provide high values of magnetic anisotropy (P%>5%), related to submagmatic and solid state deformations evolving from high to low temperature conditions. These igneous sheets are emplaced in the releasing bridge defined by two 130°E-Trending and south-dipping dextral shear zones that form a linked fault system},
publisher = {Sociedad Geológica de España},
keywords = {Dyke},
keywords = {Intrusion},
keywords = {Shear zone},
keywords = {Sanabria},
title = {Los plutones de Sotillo y Ribadelago, (Sanabria, Zamora) ejemplos de intrusiones laminares en la zona de relevo de una zona de cizalla dextra transpresiva},
title = {The Ribadelago and Sotillo plutons, examples of sheet-like intrusions in the releasing stepover of a transpressional dextral shear zone},
author = {Vegas, Néstor and Aranguren, A. and Tubía, José María},
}