U-Pb zircon geochronology of high-grade charnockites - exploration of pre-Mesoproterozoic crust in the Mazury Complex area

• Autorzy: Krzemińska Ewa , Łukawska Aleksandra , Bagiński Bogusław

Identyfikatory

DOI

10.24425/agp.2019.126445

• Języki publikacji: EN

Abstrakty

EN

Charnockites – i.e., orthopyroxene-bearing felsic rocks – were formed in a deep-seated dry environment, either under plutonic or high-grade metamorphic conditions. Most charnockites known from the crystalline basement of Poland appear to be of Mesoproterozoic age (1.50–1.54 Ga), cogenetic with the Suwałki Anorthosite Massif, and associated with mangerite and granite members forming the AMCG suite of the Mazury Complex. Genetically distinct rocks, characterised by the presence of anhydrous minerals, e.g., orthopyroxene and garnet, were also recognised along 592 m of the Łanowicze PIG-1 borehole section, within the AMCG suite. U-Pb geochronology by sensitive high resolution ion microprobe (SHRIMP) was used to date the complexly zoned zircons. The ages of crystallisation of the charnockite protoliths from various depths at 1837 ± 7, 1850 ± 9, 1842 ± 6, and 1881 ± 16 Ma makes these rocks the oldest dated crust within this part of the Polish basement. The Łanowicze PIG-1 borehole section bears components from neighbouring tectonic domains known from Lithuania: the West and Middle Lithuanian (WL/MLD) domains considered as a continental margin at 1.84–1.86 Ga and the fragmented Latvia-East Lithuania (LEL) domain, where the oldest continental crust was generated at c. 1.89–1.87 Ga. The metamorphic zircon overgrowths document a high-grade event at 1.79 Ga and then constrained at 1.5 Ga. Dating of pre-Mesoproterozoic crust cryptic within the AMCG Mazury Complex provides valuable information on the nature of the pre-existing blocks formed during the long lasting Svecofennian orogeny.

Słowa kluczowe

EN

magmatic protolith; U-Pb geochronology; dry metamorphism; continental margin

PL

protolit magmowy; geochronologia U-Pb; metamorfizm suchy; margines kontynentalny

• Wydawca: Faculty of Geology of the University of Warsaw ; Komitet Nauk Geologicznych PAN
• Czasopismo: Acta Geologica Polonica
• Rocznik: 2019
• Tom: Vol. 69, no. 4
• Strony: 489--511
• Opis fizyczny: Bibliogr 85 poz., rys., tab., wykr.

Twórcy

autor

Krzemińska Ewa

• Polish Geological Institute-National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland

autor

Łukawska Aleksandra

• Polish Geological Institute-National Research Institute, Rakowiecka 4, PL-00-975 Warszawa, Poland

autor

Bagiński Bogusław

• Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland

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Uwagi

PL

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).