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Cambro-Ordovician vs Devono-Carboniferous geodynamic evolution of the Bohemian Massif: evidence from P–T–t studies in the Orlica–Śnieżnik Dome, SW Poland

Published online by Cambridge University Press:  16 November 2017

MIROSŁAW JASTRZĘBSKI ,
BARTOSZ BUDZYŃ  and
WOJCIECH STAWIKOWSKI
MIROSŁAW JASTRZĘBSKI*
Affiliation:
Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Wrocław INGPAN, ul. Podwale 75, 50-449 Wrocław, Poland
BARTOSZ BUDZYŃ
Affiliation:
Institute of Geological Sciences, Polish Academy of Sciences, Research Centre in Kraków INGPAN, ul. Senacka 1, 31-002 Kraków, Poland
WOJCIECH STAWIKOWSKI
Affiliation:
Institute of Geology, Adam Mickiewicz University, ul. Krygowskiego 12, 61-680 Poznań, Poland
*
†Author for correspondence: mjast@interia.pl
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Abstract

The pressure–temperature–deformation–time (P–T–d–t) record of metagranitic rocks and adjacent diverse rocks of the metavolcano-sedimentary group from the Orlica–Śnieżnik Dome (OSD) in SW Poland is examined. The study aims to better understand the course of the break-up of northern Gondwana and the overprinting Variscan tectonometamorphism in the NE Bohemian Massif. We test the existing hypotheses that explain the Cambro-Ordovician thermal event recorded in the meta-supracrustal group by (i) syn-deformational regional metamorphism or (ii) the contact metamorphism of the (meta)sedimentary rocks around the intruding ~490–500 Ma granitic magmas. In addition, we check the extent and timing of the Variscan prograde and retrograde medium-pressure metamorphism in the OSD. The results imply that Early Palaeozoic monazites, rarely preserved in both rock groups, document ~490–500 Ma volcanic and plutonic events related to the Gondwana's break-up and following disturbance of the Th–U–Pb system during younger, Variscan events. The monazite geochronology reveals no distinct Cambro-Ordovician thermal aureole around the post-granitic orthogneisses. However, no large-scale Variscan juxtaposition is evident between the two main OSD rock groups or within the meta-supracrustal rocks. Consistent P–T–d–t results for the meta-supracrustal rocks and the orthogneisses suggest that their precursors contacted before the Variscan tectonometamorphism. The directly contiguous ortho- and paragneisses together experienced tectonometamorphic processes at maximum depths that correspond to 7.5–8.0 kbar and maximum temperatures of ~600–620°C, as a result of the Variscan collision of Gondwana and Euramerica. The continental collision-related events intensified at ~360 Ma and ~330–340 Ma.

Keywords

Gondwana continentCambro-Ordovician thermal eventVariscan OrogenBohemian MassifOrlica-Śnieżnik Dome
Type
Original Articles
Information
Geological Magazine , Volume 156 , Issue 3 , March 2019 , pp. 447 - 470
Copyright
Copyright © Cambridge University Press 2017 

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