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Paleomagnetism and magnetic mineralogy of metabasites and granulites from Orlica-Śnieżnik Dome (Central Sudetes)

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Abstract

The results of palaeomagnetic, rock magnetic, and microscopic study of Early Paleozoic metabasites and granulites from the OrlicaŚnieżnik Dome (OSD, Sudetes) have been combined with geochronological data. In the eastern part of the OSD (Śnieżnik Massif, SM) ferrimagnetic pyrrhotite is prevalent, accompanied by various amounts of Fe-oxides. In the western part of the OSD (Orlica-Bystrzyca Massif, OBM) Fe-oxides dominate. All magnetic minerals originated during hydrothermal and weathering processes. The palaeomagnetic study revealed the presence of three secondary components of natural remanence: Late Carboniferous, Late Permian, and Mesozoic. Two Paleozoic components are related to volcanic activity in the Sudetes. They are carried by pyrrhotite and Fe-oxides and were isolated only in SM rocks. The Mesozoic component was determined in both parts of the OSD and is carried by Fe-oxides. It covers a time span, from ∼160 to ∼40 Ma, corresponding to a long period of alteration.

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  1. Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland

    Magdalena Kądziałko-Hofmokl, Tomasz Werner & Maria Jeleńska

  2. Institute of Geological Sciences, University of Wrocław, Wrocław, Poland

    Jacek Szczepański

  3. Institute of Geochemistry, Mineralogy and Petrology, Warsaw University, Warszawa, Poland

    Krzysztof Nejbert

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  1. Magdalena Kądziałko-Hofmokl
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Correspondence to Magdalena Kądziałko-Hofmokl.

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Kądziałko-Hofmokl, M., Szczepański, J., Werner, T. et al. Paleomagnetism and magnetic mineralogy of metabasites and granulites from Orlica-Śnieżnik Dome (Central Sudetes). Acta Geophys. 61, 535–568 (2013). https://doi.org/10.2478/s11600-012-0092-y

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