MARÍA TERESA
GÓMEZ PUGNAIRE
Investigadora en el període 2020-2021
Universidad de Jaén
Jaén, EspañaPublicacions en col·laboració amb investigadors/es de Universidad de Jaén (30)
2023
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Mantle wedge oxidation from deserpentinization modulated by sediment-derived fluids
Nature Geoscience, Vol. 16, Núm. 3, pp. 268-275
2022
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Olivine-rich veins in high-pressure serpentinites: A far-field paleo-stress snapshot during subduction
Journal of Structural Geology, Vol. 163
2020
2018
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High-P metamorphism of rodingites during serpentinite dehydration (Cerro del Almirez, Southern Spain): Implications for the redox state in subduction zones
Journal of Metamorphic Geology, Vol. 36, Núm. 9, pp. 1141-1173
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U-Pb ages of detrital zircons from the Internal Betics: A key to deciphering paleogeographic provenance and tectono-stratigraphic evolution
Lithos, Vol. 318-319, pp. 244-266
2015
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Redox state of iron during high-pressure serpentinite dehydration
Contributions to Mineralogy and Petrology, Vol. 169, Núm. 4, pp. 1-18
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Subduction- and exhumation-related structures preserved in metaserpentinites and associated metasediments from the Nevado-Filábride Complex (Betic Cordillera, SE Spain)
Tectonophysics, Vol. 644, pp. 40-57
2014
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11B-rich fluids in subduction zones: The role of antigorite dehydration in subducting slabs and boron isotope heterogeneity in the mantle
Chemical Geology, Vol. 376, pp. 20-30
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FTIR and Raman spectroscopy characterization of fluorine-bearing titanian clinohumite in antigorite serpentinite and chlorite harzburgite
Earth, Planets and Space
2013
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Element mobility from seafloor serpentinization to high-pressure dehydration of antigorite in subducted serpentinite: Insights from the Cerro del Almirez ultramafic massif (southern Spain)
Lithos, Vol. 178, pp. 128-142
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Tschermak's substitution in antigorite and consequences for phase relations and water liberation in high-grade serpentinites
Lithos, Vol. 178, pp. 186-196
2012
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Late Variscan magmatism in the Nevado-Filábride Complex: U-Pb geochronologic evidence for the pre-Mesozoic nature of the deepest Betic complex (SE Spain)
Lithos, Vol. 146-147, pp. 93-111
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Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain
Earth and Planetary Science Letters, Vol. 327-328, pp. 50-60
2011
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Metamorphic record of high-pressure dehydration of antigorite serpentinite to chlorite harzburgite in a subduction setting (Cerro del Almirez, Nevado-Filábride complex, Southern Spain)
Journal of Petrology, Vol. 52, Núm. 10, pp. 2047-2078
2010
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An experimental investigation of antigorite dehydration in natural silica-enriched serpentinite
Contributions to Mineralogy and Petrology, Vol. 159, Núm. 1, pp. 25-42
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Fluid transfer into the wedge controlled by high-pressure hydrofracturing in the cold top-slab mantle
Earth and Planetary Science Letters, Vol. 297, Núm. 1-2, pp. 271-286
2009
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Breakdown mechanisms of titanclinohumite in antigorite serpentinite (Cerro del Almirez massif, S. Spain): A petrological and TEM study
Lithos, Vol. 107, Núm. 3-4, pp. 216-226
2008
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Highly ordered antigorite from Cerro del Almirez HP-HT serpentinites, SE Spain
Contributions to Mineralogy and Petrology, Vol. 156, Núm. 5, pp. 679-688
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Oriented growth of garnet by topotactic reactions and epitaxy in high-pressure, mafic garnet granulite formed by dehydration melting of metastable hornblende-gabbronorite (Jijal Complex, Kohistan Complex, north Pakistan)
Journal of Metamorphic Geology, Vol. 26, Núm. 8, pp. 855-870
2005
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Enrichment of HFSE in chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite: Implications for subduction magmatism
Geochemistry, Geophysics, Geosystems, Vol. 6, Núm. 1