Manuel
Díaz Azpiroz
Universidad de Huelva
Huelva, EspañaPublicaciones en colaboración con investigadores/as de Universidad de Huelva (27)
2021
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La influencia de los modelos cinemáticos en el análisis de tectonitas
Geotemas (Madrid), Núm. 18, pp. 50
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The southern iberian shear zone (SW Spain): Inclined transpression related to variscan oblique convergence in a ht/lp metamorphic belt
Springer Geology (Springer Science and Business Media Deutschland GmbH), pp. 137-166
2020
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Deformation mechanics in inclined, brittle-ductile transpression zones: Insights from 3D finite element modelling
Journal of Structural Geology, Vol. 137
2019
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Are we studying deformed rocks in the right sections? Best practices in the kinematic analysis of 3D deformation zones
Journal of Structural Geology, Vol. 125, pp. 218-225
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Using 3D kinematic models in subduction channels. The case of the Chañaral tectonic mélange, Coastal Cordillera, northern Chile
Gondwana Research, Vol. 74, pp. 251-270
2016
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Kinematic model of triclinic transtension zones: The case of the Boa Fé shear zone (Ossa-Morena Zone, Iberian Variscan Massif)
Geotemas (Madrid), Núm. 16, pp. 9-12
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Modelo cinemático de interacción de megacristales de feldespato alcalino durante el flujo de magmas graníticos
Geotemas (Madrid), Núm. 16, pp. 43-46
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Modelos cinemáticos de la deformación varisca en la zona de cizalla de Hiendelaencina (Anticlinorio del Ollo de Sapo, Zona Centroibérica)
Geotemas (Madrid), Núm. 16, pp. 503-506
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Structural analysis and shape-preferred orientation determination of the mélange facies in the Chañaral mélange, Las Tórtolas Formation, Coastal Cordillera, northern Chile
Journal of South American Earth Sciences, Vol. 67, pp. 40-56
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Tectonics of oblique plate boundary systems
Tectonophysics
2014
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Applying a general triclinic transpression model to highly partitioned brittle-ductile shear zones: A case study from the Torcal de Antequera massif, external Betics, Southern Spain
Journal of Structural Geology, Vol. 68, Núm. PB, pp. 316-336
2013
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Testing the model of oblique transpression with oblique extrusion in two natural cases steps and consequences
Journal of Structural Geology, Vol. 54, pp. 85-102
2012
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Fabric evidence for granodiorite emplacement with extensional shear zones in the Variscan Gredos massif (Spanish Central System)
Journal of Structural Geology, Vol. 42, pp. 74-90
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Geología de la Sierra de Huelva: una antigua sutura entre continentes
Geología de la provincia de Huelva
2011
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Deformation mechanisms of plagioclase and seismic anisotropy of the Acebuches metabasites (SW Iberian massif)
Geological Society Special Publication, Vol. 360, Núm. 1, pp. 79-95
2009
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Triclinic transpression zones with inclined extrusion
Journal of Structural Geology, Vol. 31, Núm. 10, pp. 1255-1269
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Variscan intra-orogenic extensional tectonics in the Ossa-Morena Zone (Évora-Aracena-Lora del Río metamorphic belt, SW Iberian Massif): SHRIMP zircon U-Th-Pb geochronology
Geological Society Special Publication, Vol. 327, pp. 215-237
2008
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Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone (Évora-Aracena metamorphic belt, SW Iberian Massif): Sm-Nd isotopes and SHRIMP zircon U-Th-Pb geochronology
Tectonophysics, Vol. 461, Núm. 1-4, pp. 91-113
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Quartz c-axis fabrics of poly-deformed leucocratic gneisses from the Aracena metamorphic belt (SW Variscan Chain)
Comptes Rendus - Geoscience, Vol. 340, Núm. 5, pp. 315-323
2007
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Development of lattice preferred orientation in clinoamphiboles deformed under low-pressure metamorphic conditions. A SEM/EBSD study of metabasites from the Aracena metamorphic belt (SW Spain)
Journal of Structural Geology, Vol. 29, Núm. 4, pp. 629-645