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Meliatic blueschists and their detritus in Cretaceous sediments: new data constraining tectonic evolution of the West Carpathians

  • Dušan Plašienka
  • Štefan Méres
  • Peter Ivan
  • Milan Sýkora
  • Ján Soták
  • Alexander Lačný
  • Roman Aubrecht
  • Simona Bellová
  • Tomáš Potočný
Article
  • 110 Downloads

Abstract

The Western Carpathian Meliata Superunit (Meliaticum) includes a heterogeneous group of units—the blueschist-facies Bôrka Nappe and the very low-grade chaotic complexes—polygenous mélange containing material derived from various tectonic settings (Jaklovce Unit) and Jurassic oceanic sediments with olistostrome bodies (Meliata Unit s.s.). The high pressure/low temperature (HP/LT) metamorphism, development of tectonic mélanges and synorogenic sediments took place simultaneously during the Middle–Late Jurassic in connection with closing of the Meliata Ocean. We present some new data concerning composition of variegated mélanges related to the subduction–accretion processes of the Meliata Ocean and its continental margins. The polygenous mélange contains a mixture of fragments of HP/LT up to unmetamorphosed sedimentary and volcanic rocks, including blueschist-facies radiolarites. New electron microprobe chemical age data of monazites from metasediments of the Bôrka Nappe cluster in two peaks—earliest Cretaceous ages are interpreted in terms of post-exhumation, renewed burial during formation of the Meliatic accretionary wedge. The mid-Cretaceous ages might record the thermal relaxation during the thick-skinned nappe stacking and exhumation of the neighbouring Veporic metamorphic dome. In addition, we describe two distinct types of tourmalines and epidotes occurring in the Bôrka blueschists that document the prograde HP and retrograde LP metamorphic events. Detritus of the blueschist-facies rocks appears for the first time in the heavy mineral spectra of the Barremian–Aptian platform limestones. These limestones occur as clasts, together with glaucophanite pebbles, in the Albian–Cenomanian flysch formations of the Pieniny Klippen Belt (Klape Unit). We also review occurrences of other blueschist and ophiolitic erosional products in Cretaceous clastic formations and suggest that all have a Meliatic provenance.

Keywords

Meliata Ocean High pressure/low temperature metamorphism Mélange Olistostrome Radiolarite Monazite dating Heavy minerals 

Notes

Acknowledgements

The authors appreciate the financial support from the Grant Agency for Science, Slovakia (projects VEGA 1/0085/17 and 2/0034/16) and from the Slovak Research and Development Agency (projects APVV-0212-12 and APVV-17-0170). The authors are indebted to László Fodor and an anonymous reviewer for their valuable comments and suggestions that helped to improve the scientific content a readability of the earlier version of the manuscript. The same applies to the editorial comments of Edwin Gnos and Stefan Schmid. The analyzed samples are stored at the Department of Geology and Palaeontology and Department of Geochemistry, Faculty of Natural Sciences, Comenius University in Bratislava, and at the Earth Science Institute of the Slovak Academy of Sciences in Banská Bystrica.

Supplementary material

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© Swiss Geological Society 2018

Authors and Affiliations

  1. 1.Department of Geology and Palaeontology, Faculty of Natural SciencesComenius UniversityBratislavaSlovakia
  2. 2.Department of Geochemistry, Faculty of Natural SciencesComenius UniversityBratislavaSlovakia
  3. 3.Earth Science Institute of the Slovak Academy of SciencesBratislavaSlovakia

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