BENITO
ABALOS VILLARO
PROFESORADO CATEDRATICO/A DE UNIVERSIDAD
Publications (121) BENITO ABALOS VILLARO publications View referenced research data.
2025
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Hybridization of crustal magmas and direct evidence for two mantle sources during Early-Ordovician magmatism at the NW Gondwana margin
Lithos, Vol. 514-515
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LiDAR mapping of the sedimentary rocks surrounding a salt diapir: a powerful tool to assist landslide identification and structural/depositional sequence analysis (Maestu diapir, N Spain)
Journal of Maps, Vol. 21, Núm. 1
2024
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Correction to: The crystalline quartz-rich raw material from Olduvai Gorge (Tanzania): why is it called quartzite when it should be called quartz? (Archaeological and Anthropological Sciences, (2023), 15, 6, (78), 10.1007/s12520-023-01774-9)
Archaeological and Anthropological Sciences
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Geochronological record of Cadomian exterior orogen reworking in bi-modal igneous protoliths of the Cabo Ortegal Allochthon (NW Iberia): the Cambrian onset of the Palaeozoic plate-tectonic cycle
International Geology Review, Vol. 66, Núm. 1, pp. 310-335
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Petrofabric and Raman microspectroscopy study of the Mina Afortunada gneiss dome: Mapping its thermal gradient
Journal of Structural Geology, Vol. 187
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The Neoproterozoic Mozambique Belt in the Gol Mountains (N Tanzania): Structural Analysis of Amphibolite and Granulite-Facies Nappe Tectonites From a Crustal Orogenic Channel
Tectonics, Vol. 43, Núm. 11
2023
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Low–Ti Continental Tholeiite Origin of Magmas With Calc-Alkaline Signature in Transcurrent Settings: The Mississippian Matachel Volcanic Field (SW Iberian Massif)
Geochemistry, Geophysics, Geosystems, Vol. 24, Núm. 11
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Mineral chemistry dataset of the Tournaisian – Lower Viséan submarine basaltic volcanism of the Matachel Basin (SW Iberian Massif).
Data in Brief
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Pleistocene river diversions caused by large landslides in the western Pyrenees (Oria River drainage basin, N Spain)
Basin Research, Vol. 35, Núm. 6, pp. 2268-2300
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Polyphase tectonic reworking of serpentinites and chlorite-tremolite-talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement
Journal of Metamorphic Geology, Vol. 41, Núm. 4, pp. 491-523
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The crystalline quartz-rich raw material from Olduvai Gorge (Tanzania): why is it called quartzite when it should be called quartz?
Archaeological and Anthropological Sciences, Vol. 15, Núm. 6
2022
2020
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Corrigendum to ‘Ediacaran - Earliest Cambrian arc-tholeiite and adakite associations of the Malcocinado Formation (Ossa-Morena Zone, SW Spain): juvenile continental crust and deep crustal reworking in northern Gondwana’. [Lithos 372–373 (2020) 105683] (LITHOS (2020) 372–373, (S0024493720303200), (10.1016/j.lithos.2020.105683))
Lithos
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Ediacaran - Earliest Cambrian arc-tholeiite and adakite associations of the Malcocinado Formation (Ossa-Morena Zone, SW Spain): Juvenile continental crust and deep crustal reworking in northern Gondwana
Lithos, Vol. 372-373
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U-Pb, Hf isotope and REE constraints on high-pressure acid migmatites from the Cabo Ortegal Complex (NW Spain): New evidence of short-duration metamorphism in a Variscan subduction channel
Lithos, Vol. 372-373
2019
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Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
International Journal of Earth Sciences, Vol. 108, Núm. 6, pp. 2037-2046
2018
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Boris Choubert: Unrecognized visionary geologist, pioneer of the global tectonics
Bulletin de la Societe Geologique de France, Vol. 189, Núm. 2
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Crustal xenoliths from the Calatrava Volcanic Field: a petrofabric and geochronological study.
Macla: revista de la Sociedad Española de Mineralogía, Núm. 23
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Petrofabric of forsterite marbles and related rocks from a low-pressure metamorphic terrain (Almadén de la Plata massif, Ossa-Morena Zone, SW Spain) and its kinematic interpretation
Journal of Structural Geology, Vol. 117, pp. 58-80
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Scales of deformation partitioning during exhumation in a continental subduction channel: A petrofabric study of eclogites and gneisses from NW Spain (Malpica-Tui Allochthonous Complex)
Journal of Metamorphic Geology, Vol. 36, Núm. 2, pp. 225-254