The Orlica–Śnieżnik Dome, the Sudetes, in 2002 and 12 years later

Żelaźniewicz, A.; Jastrzębski, M.; Redlińska-Marczyńska, A.; Szczepański, J.

Artykuł - szczegóły

Tytuł artykułu

The Orlica–Śnieżnik Dome, the Sudetes, in 2002 and 12 years later

Autorzy

Żelaźniewicz A. , Jastrzębski M. , Redlińska-Marczyńska A. , Szczepański J.

Wybrane pełne teksty z tego czasopisma

http://geojournals.pgi.gov.pl/gs/index

Identyfikatory

Warianty tytułu

Języki publikacji

Abstrakty

During the 2002 meeting of Czech, Polish and Slovak tectonic community in Żelazno, the Sudetes, the Central European Tectonic Studies Group (CETeG) was established. 12 years ago, participants of the meeting made an excursion to the eastern part of the Orlica–Śnieżnik Dome (OSD), which was focused on a variety of gneisses with inserts of (U)HP eclogites and various enclaves. The 2014 meeting brought members of the CETeG to the OSD again and an accompanying field excursion was dedicated mainly to evolution of metasedimentary and metavolcanogenic rocks in the region. This paper is a short review of the results of the studies undertaken in the OSD by different research groups in the last 12 years. The review is set against a background of what we knew about the geology of the dome in 2002. A significant progress was made. P-T paths were determined for mica schists and marbles as well as for metarhyolites originated from the continental crust and metabasites derived from the mantle. New light was shed on the origin of various types gneisses in the OSD and their genetic and structural relationships. A plethora of isotopic studies helped to better constrain timing of igneous and metamorphic events in the Orlica–Śnieżnik complex. Ages clustered around 350–340 Ma are repeatedly obtained, yet scarcer older ages up to 390 Ma and their geological significance are open to debate. Tectonic evolution of the dome was revised and new geodynamic concepts were proposed. However the new data has created some new problems and some old problems are still to be resolved in the future.

Słowa kluczowe

Orlica-Śnieżnik Dome eclogite granite migmatite mica schist orthogneiss Variscan orogen bimodal volcanism

Wydawca

Instytut Nauk Geologicznych PAN
Instytut Nauk Geologicznych Uniwersytetu Wrocławskiego

Czasopismo

Geologia Sudetica

Rocznik

2014

Tom

Vol. 42

Strony

105--123

Opis fizyczny

Bibliogr. 141 poz., rys., tab.

Twórcy

autor

Żelaźniewicz A.

pansudet@pwr.wroc.pl

Instytut Nauk Geologicznych PAN, Podwale 75, 50-449 Wrocław, Poland
Instytut Geologii, Uniwersytet Adama Mickiewicza, ul Maków Polnych 16, 61-606 Poznań

autor

Jastrzębski M.

mjast@interia.pl

Instytut Nauk Geologicznych PAN, Podwale 75, 50-449 Wrocław, Poland

autor

Redlińska-Marczyńska A.

aleksandra.redlinska-marczynska@amu.edu.pl

Instytut Geologii, Uniwersytet Adama Mickiewicza, ul Maków Polnych 16, 61-606 Poznań

autor

Szczepański J.

js@ing.uni.wroc.pl

Instytut Nauk Geologicznych, Uniwersytet Wrocławski, Maxa Borna 9, 50-204 Wrocław

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