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Publications

Publications

  1. Chaves, A.O., Ernst, R.E., Söderlund, U., Wang, X., Næraa, T. (2018). The 920-900 Ma Bahia-Gangila lip of the São Francisco and Congo cratons and link with Dashigou-Chulan lip of North China craton: New insights from U-Pb geochronology and geochemistry. Precambrian research, available online 31 August.
  2. Limburg, K.E., Wuenschel, M.J., Hüssy, K., Heimbrand, Y., Samson M. (2018).  Making the otolith magnesium chemical calendar-clock tick: plausible mechanism and supporting evidence.  Reviews in Fisheries Science and Aquaculture 26: 479-493. doi: 10.1080/23308249.2018.1458817.
  3. Rey-Solé, M., Scherstén, A., Næraa, T., Olausson, D. & Mangado, X. (2017). Siliceous Raw Material Exploitation at Hort de la Boquera Site (Margalef de Monsant, Tarragona, España): First Results from LA-ICP-MS Analysis. in Pereira, Terradas & Bicho (eds), The Exploitation of Raw Materials in Prehistory: Sourcing, Processing and Distribution. Cambridge Scholars Publishing, Newcastle upon Tyne, pp. 234-249.
  4. Næraa, T., Kokfelt, T.F., Thrane, K. (2016). Geochronology of the larger Skjoldungen area South-East Greenland (62° 30’ - 64° N). Danmarks og Grønlands Geologiske Undersøgelse Rapport 2016/39, 74 pp.
  5. Kokfelt, T.F., Næraa, T., Thrane, K., Bagas, L. (2016). New Zircon U-Pb and Hf isotopic constraints on the crustal evolution of the Skjoldungen region, South-East Greenland. Geological Survey of Denmark and Greenland Bulletin 35, 55-58

Conference abstracts

  1. Næraa, T., Scherstén, A., Ingered, M. (2018). Using rectangular spot shapes for LA-ICP-MS zircon U-Pb age dating. European Workshop on Laser Ablation (EWLA 2018), conference abstract.
  2. Heimbrand, Y., Limburg, K. (2018). Losing track of time: Dubious age determination of Baltic cod, probable causes and promising solution. 6th international otolith symposium, conference abstrace
  3. Herrmann et al., (2018) LA-ICP-MS U-Pb Dating of Shocked Zircons of Siljan Impact Structure, Sweden - Impact-related Ages or Post-impact Hydrothermal Pb loss? 81st Annual Meeting of the Meteoritical-Society.
  4. Ni et al., (2018). Tracing hypoxia in the Baltic Sea during the Holocene using foraminifera-based geochemistry and faunal assemblages. Forams 2018 Conference.
  5. Möller, C., Klonowska, I., Johansson, L., Janák, M, Majka, J., Næraa, T. (2017). Microdiamond-bearing meta-supracrustal rocks in Roan, northernmost Western Gneiss Region, Scandinavian Caledonides. International Eclogite Conference.
  6. Ni et al., (2017). Tracing hypoxia in the Baltic Sea using trace elemental geochemistry and  and foraminiferal faunal assemblages. Goldsmith conference abstract.
  7. Hansen, E.C., Johansson, L., Næraa, T. (2016). Whole-rock and mineral chemistry of calcsilicate lenses within mafic gneisses in a high-grade metamorphic terrane, Halland Province Sweden. Geological Society of America, Annual meeting, conference abstract.
  8. Rey -Solé, M., Scherstén, A., Næraa, T., Olausson, D., Mangado, X. (2016). Siliceous raw materials exploitation at Hort de la Boquera site (Margalef de Montsant, Tarragona, España): first approaches on ICP-MS-LA analysis. Raw materials exploitation in Prehistory: Sourcing, processing and distribution, conference abstract

Published student projects (bachelor and master)

  1. Dynamic Recrystallization in the Sveconorwegian Frontal Wedge, Småland, southern Sweden. Report number 547, 2018, by Jesper Perälä.
  2. Stratigraphy  and  pyrite  geochemistry of  the  Lower-Upper  Ordovician  in  the Lerhamn  and  Fågelsång-3  drill  cores, Scania, Sweden. Report number 530, 2018, by Fisnik Balija.
  3. New geochronological constraints on the Klipriviersberg Group: defining a new Neoarchean large igneous province on the Kaapvaal Craton, South Africa. Report number 524, 2017, by Joän Stamsnijder.
  4. U-Pb datering av zirkon från migmatitisk gnejs i Delsjöområdet, Idefjordenterrängen. Report number 512, 2017, by Mimmi Ingerid.
  5. Depositional history of the Neoproterozoic Visingsö Group, south-central Sweden. Report number 504, 2017, by Viktor Ahrenstedt
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