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Polymetamorphic evolution of pelites inferred from tourmaline zoning – the Rędziny hornfels case study at the eastern contact of the Karkonosze Granite, Sudetes, Poland Cover

Polymetamorphic evolution of pelites inferred from tourmaline zoning – the Rędziny hornfels case study at the eastern contact of the Karkonosze Granite, Sudetes, Poland

Open Access
|Mar 2019

Authors

Jarosław Majka

jaroslaw.majka@geo.uu.se

AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, Kraków, Poland
Uppsala University, Department of Earth Sciences, Uppsala, Sweden

Mateusz P. Sęk

AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, Kraków, Poland

Stanisław Mazur

Polish Academy of Sciences, Institute of Geological Sciences, Kraków, Poland

Bożena Gołębiowska

AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, Kraków, Poland

Adam Pieczka

AGH University of Science and Technology, Department of Mineralogy, Petrography and Geochemistry, Kraków, Poland
DOI: https://doi.org/10.2478/mipo-2018-0003 | Journal eISSN: 1899-8526 | Journal ISSN: 1899-8291
Language: English
Page range: 17 - 34
Submitted on: Apr 20, 2017
Accepted on: Dec 10, 2017
Published on: Mar 2, 2019
Published by: Mineralogical Society of Poland
In partnership with: Paradigm Publishing Services
Publication frequency: 1 issue per year

© 2019 Jarosław Majka, Mateusz P. Sęk, Stanisław Mazur, Bożena Gołębiowska, Adam Pieczka, published by Mineralogical Society of Poland
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.