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Nuevas evidencias de metamorfismo de alta presión en el Alóctono Inferior de Trás-os-Montes (N Portugal)
Ayuda Buscar en la ayuda Buscar en la ayuda Nuevas evidencias de metamorfismo de alta presión en el Alóctono Inferior de Trás-os-Montes (N Portugal) J.I. Gil Ibarguchi [1] ; S. García de Madinabeitia [1] ; P. Puelles [1] ; M.L. Ribeiro [2] [1] Universidad del País Vasco [2] LNEG – Laboratorio Nacional de Energia e Geologia, Portugal Localización: Geotemas (Madrid), ISSN 1576-5172, Nº. 20, 2024 (Ejemplar dedicado a: XI Congreso Geológico de España), pág.
Dehydration of subducting slow-spread oceanic lithosphere in the Lesser Antilles
The inversion was carried out in a local Cartesian reference frame with origin at 61° W, 16° N and rotated by 24° to align the x axis perpendicular to the strike of the trench. The starting P-wave velocity model was built as a pseudo-1D hanging model (a 3D model built by ‘hanging’ a single velocity/depth profile below a given surface) referenced to the depth of the crystalline basement, which was constrained by MCS profiles39,40,41.
Eclogite inclusions from subducted metaigneous continental crust (Malpica-Tui Allochthonous Complex, NW Spain): petrofabric, geochronology and calculated seismic properties - Puelles - 2017 - Tectonics - Wiley Online Library
This study describes the strain geometry, crystal-plastic deformational features, isotopic age of metamorphism, and calculated seismic properties of two medium-temperature eclogite types from the Malpica-Tui Allochthonous Complex of Variscan NW Iberia. The eclogite types are eclogites with coronitic garnets and eclogites with a planolinear fabric.
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