JANE HANNAH
SCARROW
PROFESORA TITULAR DE UNIVERSIDAD
FERNANDO
BEA BARREDO
Ikertzailea null-(e)tik
FERNANDO BEA BARREDO-rekin lankidetzan egindako argitalpenak (30)
2021
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Contrasting high-Mg, high-K rocks in Central Iberia: the appinite—vaugnerite conundrum and their (non-existent) relation with arc magmatism
Journal of Iberian Geology, Vol. 47, Núm. 1-2, pp. 235-261
2018
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Lu-Hf ratios of crustal rocks and their bearing on zircon Hf isotope model ages: The effects of accessories
Chemical Geology, Vol. 484, pp. 179-190
2017
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Palaeogeography and crustal evolution of the Ossa–Morena Zone, southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: a review of isotopic evidence
International Geology Review, Vol. 59, Núm. 1, pp. 94-130
2016
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Caracterización del basamento Bético: Un estudio U-Th-Pb SHRIMP en circones de enclaves graníticos Variscos incluidos en lamproítas de la Región Volcánica Neógena del sureste de España
Geotemas (Madrid), Núm. 16, pp. 27-30
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Mineralogical evidence for lamproite magma mixing and storage at mantle depths: Socovos fault lamproites, SE Spain
Lithos, Vol. 266-267, pp. 182-201
2015
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The spatial and compositional evolution of the Late Jurassic Ghorveh-Dehgolan plutons of the Zagros Orogen, Iran: SHRIMP zircon U-Pb and Sr and Nd isotope evidence
Geologica acta: an international earth science journal, Vol. 13, Núm. 1, pp. 25-43
2014
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Creación de un e-book de prácticas de Petrología (PID 12-213)
Innovación docente y buenas prácticas en la Universidad de Granada: Vol. 3 (Editorial Universidad de Granada), pp. 746-757
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Kalsilite-bearing plutonic rocks: The deep-seated Archean Awsard massif of the Reguibat Rise, South Morocco, West African Craton
Earth-Science Reviews, Vol. 138, pp. 1-24
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Unraveling sources of A-type magmas in juvenile continental crust: Constraints from compositionally diverse Ediacaran post-collisional granitoids in the Katerina Ring Complex, southern Sinai, Egypt
Lithos, Vol. 192-195, pp. 56-85
2012
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Anomalous xenocryst dispersion during tonalite-granodiorite crystal mush hybridization in the mid crust: Mineralogical and geochemical evidence from Variscan appinites (Avila Batholith, Central Iberia)
Lithos, Vol. 153, pp. 224-242
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Condiciones P-T de formación de asociaciones con Cl-anfíbol en gneises leucocráticos del complejo meta-ígneo Precámbrico de Gebel Kamil (EgiptoSudán): implicaciones para el origen de fluidos salinos en la corteza inferior
Geotemas (Madrid), Núm. 13, pp. 898-901
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On the Seventh Hutton Symposium on the origin of granites and related rocks
Lithos
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SHRIMP U-Pb zircon dating of the Katerina Ring Complex: Insights into the temporal sequence of Ediacaran calc-alkaline to peralkaline magmatism in southern Sinai, Egypt
Gondwana Research, Vol. 21, Núm. 4, pp. 887-900
2011
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Lamprophyre dikes as tectonic markers of late orogenic transtension timing and kinematics: A case study from the Central Iberian Zone
Tectonics, Vol. 30, Núm. 4
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The Bir Safsaf Precambrian inlier of South West Egypt revisited. A model for ~1.5Ga TDM late Pan-African granite generation by crustal reworking
Lithos, Vol. 125, Núm. 3-4, pp. 897-914
2010
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The palaeogeographic position of Central Iberia in Gondwana during the Ordovician: Evidence from zircon chronology and Nd isotopes
Terra Nova, Vol. 22, Núm. 5, pp. 341-346
2009
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Erratum: Shoshonites, vaugnerites and potassic lamprophyres: Similarities and differences between 'ultra'-high-K rocks (Earth and Environmental Science Transactions of the Royal Society of Edinburgh (2009) 99 (159-175) DOI: 10.1017/S1755691009008032)
Earth and Environmental Science Transactions of the Royal Society of Edinburgh
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High-Ti amphibole as a petrgenetic indicator of magma chemistry: Evidence for mildly alkalic-hybrid melts during evolution of Variscan basic-ultrabasic magmatism of Central Iberia
Contributions to Mineralogy and Petrology, Vol. 158, Núm. 1, pp. 69-98
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Reply to discussion on the Eocene bimodal Piranshahr massif of the Sanadaj-Sirjan Zone, West Iran: A marker of the end of collision in the Zagros orogen
Journal of the Geological Society, Vol. 166, Núm. 5, pp. 983-984
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The Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan Zone, NW Iran: A marker of the end of the collision in the Zagros orogen
Journal of the Geological Society, Vol. 166, Núm. 1, pp. 53-69