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  • 1. Majka, Jarosław
    et al.
    Mazur, Stanisław
    Młynarska, Maria
    Klonowska, Iwona
    Tual, Lorraine
    Swedish Museum of Natural History, Department of Geology.
    Kośmińska, Karolina
    Tarasiuk, Jacek
    Wroński, Sebastian
    Integrating X‐ray mapping and microtomography of garnet with thermobarometry to define the P–T evolution of the (near) UHP Międzygórze eclogite, Sudetes, SW Poland2018In: Journal of Metamorphic Geology, ISSN 0263-4929, E-ISSN 1525-1314Article in journal (Refereed)
  • 2.
    Petersson, Andreas
    et al.
    Swedish Museum of Natural History, Department of Geology.
    Tual, Lorraine
    Swedish Museum of Natural History, Department of Geology.
    Zircon U-Pb-Hf isotope data in eclogite and metagabbro from southern Sweden reveal a common long-lived evolution and enriched source2020In: GFF, ISSN 1103-5897, E-ISSN 2000-0863, Vol. 142, no 4, p. 253-266Article in journal (Refereed)
    Abstract [en]

    Several orogenies have shaped the bedrock of southern Sweden. While mafic intrusions represent significant sources of information for reconstructing geodynamics and crustal evolution, the characterization of the various generations of such intrusions in Sweden remains limited. We reportin situzircon U-Pb ages and Hf isotope data from a Fe-Ti eclogite and a coronitic metagabbro from the Eastern Segment in southern Sweden. Crystallisation ages at 1683 +/- 17 Ma of the eclogite suggest affiliation with the surrounding 1730-1660 Ma Transscandinavian Igneous Belt intrusions that dominate the Eastern Segment. Secondary zircon growth and Pb-loss in the eclogite sample at 1459 +/- 44 Ma and the crystallisation of the metagabbro at 1431 +/- 26 Ma overlap and are related to magmatic activity during the Hallandian orogeny. Zircon Hf isotope signatures with chondritic and sub-chondritic values at similar to 1683 Ma and similar to 1431 Ma, respectively, correspond to an enriched (or mildly depleted) source in line with a "Mixed Svecofennian Crustal Reservoir". These isotope signatures are more enriched than those in the surrounding gneisses. Zircon isotope data from the herein analysed zircon grains indicate that the eclogite and metagabbro had an enriched mafic source in the mid to lower crust, or within the subcontinental lithospheric mantle below Fennoscandia.

  • 3.
    Tual, Lorraine
    et al.
    Swedish Museum of Natural History, Department of Geology. Department of Geology, Lund University, Sweden.
    Möller, Charlotte
    Department of Geology, Lund University, Sweden.
    Whitehouse, Martin
    Swedish Museum of Natural History, Department of Geology.
    Tracking the prograde P–T path of Precambrian eclogite using Ti-in-quartz and Zr-in-rutile geothermobarometry2018In: Contributions to Mineralogy and Petrology, Vol. 173, no 7, article id 56Article in journal (Refereed)
  • 4.
    Tual, Lorraine
    et al.
    Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden.
    Piñán-Llamas, Aránzazu
    Department of Geosciences, IPFW University, 2101 E. Coliseum Blvd, Fort Wayne, IN 46805, USA.
    Möller, Charlotte
    Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden.
    High-temperature deformation in the basal shear zone of an eclogite-bearing fold nappe, Sveconorwegian orogen, Sweden2015In: Precambrian Research, ISSN 0301-9268, E-ISSN 1872-7433, Vol. 265, p. 104-120Article in journal (Refereed)
  • 5.
    Tual, Lorraine
    et al.
    Department of Geosciences Swedish Museum of Natural History Stockholm Sweden;Department of Earth, Ocean, and Atmospheric Sciences University of British Columbia Vancouver Canada.
    Smit, Matthijs A.
    Department of Earth, Ocean, and Atmospheric Sciences University of British Columbia Vancouver Canada.
    Kooijman, Ellen
    Swedish Museum of Natural History, Department of Geology. Department of Geosciences Swedish Museum of Natural History Stockholm Sweden.
    Kielman-Schmitt, Melanie
    Swedish Museum of Natural History, Department of Geology.
    Ratschbacher, Lothar
    Geologie TU Bergakademie Freiberg Freiberg Germany.
    Garnet, zircon, and monazite age and REE signatures in (ultra)high‐temperature and high‐pressure rocks: Examples from the Caledonides and the Pamir2022In: Journal of Metamorphic Geology, ISSN 0263-4929, E-ISSN 1525-1314, Vol. 40, no 8, p. 1321-1346Article in journal (Refereed)
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