Wstępna charakterystyka pierwiastków ziem rzadkich i innych pierwiastków śladowych w osadach drobnoziarnistych z pogranicza triasu i jury w dawnej bruździe śródpolskiej

• Autorzy: Brański P.

Identyfikatory

DOI

10.5604/01.3001.0012.6916

Warianty tytułu

EN

Preliminary characteristics of rare earth elements and other trace elements in fine-grained deposits from the Triassic-Jurassic transition in the former Mid-Polish Trough

• Konferencja: Kongres surowcowy = Raw materials congress : 5. Konferencja: Złoża kopalin - aktualne problemy prac poszukiwawczych, badawczych i dokumentacyjnych = 5th Conference: Natural resources - current problems of prospection, exploration and documentation ; 28. Konferencja: Aktualia i perspektywy gospodarki surowcami mineralnymi = 28th Conference: Updates and prospects of mineral resources management / pod red. nauk. Stanisława Z. Mikulskiego
• Języki publikacji: PL

Abstrakty

PL

Skały drobnoklastyczne z pogranicza triasu i jury (retyk–hetang), nagromadzone w dawnej bruździe śródpolskiej były przedmiotem badań geochemicznych w Państwowym Instytucie Geologicznym – Państwowym Instytucie Badawczym w Warszawie. 94 próbki iłowców i mułowców, pochodzące z sześciu archiwalnych rdzeni wiertniczych, przeanalizowano metodami ICP-MS i XRF, na zawartość pierwiastków ziem rzadkich (REE) i innych pierwiastków śladowych. Wyniki wskazują, że źródłem większości badanych mułowców i iłowców były skały osadowe górnej skorupy kontynentalnej starych obszarów kratonicznych, których protolit miał charakter umiarkowanie felzytowy. Procesy wietrzenia i recyklingu zmodyfikowały, do pewnego stopnia, pierwotny skład chemiczny. Jednak w retyku i wczesnym hetangu, w południowo-wschodnim segmencie bruzdy, niektóre dane geochemiczne sugerują większą dostawę z wulkanicznego protolitu o charakterze maficznym. Ponadto, w kilku próbkach zaobserwowano wyraźne wzbogacenie w pierwiastki ziem rzadkich, w wyniku domieszki minerałów akcesorycznych, będących głównymi nośnikami REE. Tym niemniej, na podstawie obecnie otrzymanych wyników, koncentracje REE (i innych pierwiastków śladowych) w bruździe śródpolskiej są niskie i mają one naukowe znaczenie wskaźnikowe, natomiast nie mają znaczenia surowcowego.

EN

Fine-grained siliciclastic rocks from the Triassic-Jurassic transition (Rhaetian–Hettangian) in the former Mid-Polish Trough were the subject of the geochemical study at the Polish Geological Institute – National Research Institute in Warsaw. Ninety-four samples of claystones and mudstones from six archived drill cores were analysed by ICP-MS and XRF for rare earth elements (REE) and other trace elements. The results indicate that the sources of most of the claystones and mudstones were sedimentary rocks of the upper continental crust of old cratonic areas, where the protolith had a moderately felsic character. Weathering and recycling processes modified the original chemical composition to some extent. However, during Rhaetian and early Hettangian, some geochemical data in the south-eastern segment of the MPT suggest significant input from a mafic volcanic protolith. Moreover, a clear enrichment in rare-earth elements was observed in few samples, caused by admixtures of accessory minerals (being a main carrier of REE). Nevertheless, based on currently obtained data, the Rhaetian–Hettangian concentrations of REE (and other trace elements) in the MPT are low and they are of scientific indicative significance, not of raw material importance.

Słowa kluczowe

PL

pierwiastki śladowe i REE; proweniencja; wietrzenie i recykling; drobnoziarniste skały silikoklastyczne; pogranicze trias–jura; bruzda śródpolska

EN

trace elements and REE; provenance; weathering and recycling; fine-grained siliciclastic rocks; Triassic–Jurassic transition; Mid-Polish Trough

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Biuletyn Państwowego Instytutu Geologicznego
• Rocznik: 2018
• Tom: nr 472
• Strony: 255--270
• Opis fizyczny: Bibliogr. 50 poz., rys., tab., wykr.

Twórcy

autor

Brański P.

• Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy, ul. Rakowiecka 4, 00-975 Warszawa

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