Research Article| December 01, 2014 Microdiamond discovered in the Seve Nappe (Scandinavian Caledonides) and its exhumation by the “vacuum-cleaner” mechanism Jarosław Majka; Jarosław Majka 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Search for other works by this author on: GSW Google Scholar Åke Rosén; Åke Rosén 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Search for other works by this author on: GSW Google Scholar Marian Janák; Marian Janák 2Slovak Academy of Sciences, Geological Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic Search for other works by this author on: GSW Google Scholar Nikolaus Froitzheim; Nikolaus Froitzheim 3University of Bonn, Steinmann-Institut, Poppelsdorfer Schloss, 53115 Bonn, Germany Search for other works by this author on: GSW Google Scholar Iwona Klonowska; Iwona Klonowska 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Search for other works by this author on: GSW Google Scholar Maciej Manecki; Maciej Manecki 4AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, al. Mickiewicza 30, 30-059 Krakow, Poland Search for other works by this author on: GSW Google Scholar Vlasta Sasinková; Vlasta Sasinková 5Slovak Academy of Sciences, Institute of Chemistry, Dúbravská 9, 840 05 Bratislava, Slovak Republic Search for other works by this author on: GSW Google Scholar Kenta Yoshida Kenta Yoshida 6Kyoto University, Graduate School of Science, Department of Geology and Mineralogy, Kyoto 606-8502, Japan Search for other works by this author on: GSW Google Scholar Author and Article Information Jarosław Majka 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Åke Rosén 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Marian Janák 2Slovak Academy of Sciences, Geological Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic Nikolaus Froitzheim 3University of Bonn, Steinmann-Institut, Poppelsdorfer Schloss, 53115 Bonn, Germany Iwona Klonowska 1Uppsala University, Department of Earth Sciences, CEMPEG, Villavägen 16, 752-36 Uppsala, Sweden Maciej Manecki 4AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, al. Mickiewicza 30, 30-059 Krakow, Poland Vlasta Sasinková 5Slovak Academy of Sciences, Institute of Chemistry, Dúbravská 9, 840 05 Bratislava, Slovak Republic Kenta Yoshida 6Kyoto University, Graduate School of Science, Department of Geology and Mineralogy, Kyoto 606-8502, Japan Publisher: Geological Society of America Received: 24 Jul 2014 Revision Received: 25 Sep 2014 Accepted: 02 Oct 2014 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2014 Geological Society of America Geology (2014) 42 (12): 1107–1110. https://doi.org/10.1130/G36108.1 Article history Received: 24 Jul 2014 Revision Received: 25 Sep 2014 Accepted: 02 Oct 2014 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jarosław Majka, Åke Rosén, Marian Janák, Nikolaus Froitzheim, Iwona Klonowska, Maciej Manecki, Vlasta Sasinková, Kenta Yoshida; Microdiamond discovered in the Seve Nappe (Scandinavian Caledonides) and its exhumation by the “vacuum-cleaner” mechanism. Geology 2014;; 42 (12): 1107–1110. doi: https://doi.org/10.1130/G36108.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract When a continent collides with an island arc or other continent, continental crust of the subducted continent may be buried to depths exceeding 100 km, and exposed to pressures that can cause formation of coesite and diamond. This process leads to substantial density increase in SiO2-rich rocks and, in turn, to a reduction of the buoyancy of the subducted material, which should inhibit exhumation. Nevertheless, coesite- and diamond-bearing continental crustal rocks are known from several occurrences worldwide. We report on the discovery of microdiamond in kyanite-garnet gneiss from allochthonous metasediments of the Seve Nappe Complex in the Scandinavian Caledonides. Our discovery calls for general reconsideration of existing exhumation models of deeply subducted continental crust. We propose that the diamond-bearing rocks were subducted in an arc-continent collision setting, and their exhumation was facilitated by local pressure reduction resulting from extraction of the forearc lithospheric block. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Read full abstract