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Ophiolitic blocks, represented by metagabbro and serpentinite containing relict pyroxene, olivine, baddeleyite, zirconolite, Ni-pyrite and pyrrhotite, were found as exotic blocks in an olistostrome in the Magura Nappe, Outer Western Carpathians. The geochemical and isotopic features of the blocks suggest they represent mantle-derived rocks, with within-plate geochemistry signatures, modified by subduction, with lithospheric mantle input. A U-Pb apatite cooling age (614 ±3 Ma) is within age uncertainty of a published U-Pb zircon magmatic crystallization age (~614 Ma) implying rapid post-crystallization cooling. Pervasive alteration with replacement of primary minerals by low-temperature assemblages is observed in all rock fragments and is interpreted as contemporaneous with shearing. The secondary mineral assemblages and temperature modelling allow the interpretation that the pervasive ocean-floor metamorphism is the alteration in these meta-mafic rocks. These ophiolitic fragments can be linked to the Neoproterozoic break up of Rodinia/Pannotia.
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art. no. 9
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Bibliogr. 89 poz., rys., tab., wykr.
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- University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
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- University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
autor
- Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Al. Mickiewicza 30, 20-059 Kraków, Poland
autor
- Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Al. Mickiewicza 30, 20-059 Kraków, Poland
autor
- University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
autor
- M.P. Semenenko Institute of Mineralogy, Geochemistry and Ore Formation of the National Academy of Sciences of Ukraine, Palladina 34, Kyiv-142, Ukraine
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2b749629-7a44-48c8-981c-c0ca96280172