Ancylite-(Ce) from quartz-calcite-chlorite veins in phyllite of the Opava Mountains (SW Poland)

• Autorzy: Janeczek Janusz , Szopa Krzysztof , Fabiańska Monika

Identyfikatory

DOI

10.7306/gq.1550

• Języki publikacji: EN

Abstrakty

EN

Ancylite-(Ce) occurs in quartz-calcite-chlorite veins crosscutting the foliation of phyllite in the Dewon Quarry in the foothills of the Opava Mountains of the eastern Sudetes, south-west Poland. Irregularly shaped grains of ancylite are up to 67 μm long and 22 μm wide. The compositional range of ancylite, determined by electron microprobe, is expressed by the empirical formula: (Sr_0.65-0.55Ca_0.19-0.14Fe_0.03-0.00)_∑0.87-0.69 (Ce_0.58-0.50Nd_0.26-0.22La_0.26-0.21Pr_0.06-0.05Sm_0.05-0.04Gd_0.07-0.03Dy_0.01-0.00)_∑1.29-1.05 (CO₃)₂(OH_1.07-0.99F_0.22-0.0.06)_∑1.29-1.05· 0.95-0.93H₂O. Ancylite crystallized directly from CO₂-rich hydrothermal solutions as the last mineral in the veins following precipitation of calcite. The solution temperature, estimated using various chlorite geothermometres, was in the range of 260-340°C.

Słowa kluczowe

EN

ancylite-(Ce); phyllite; CO2-rich hydrothermal solution; Opava Mts.; Poland

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2020
• Tom: Vol. 64, No. 3
• Strony: 801--806
• Opis fizyczny: Bibliogr. 37 poz., fot., rys., wykr.

Twórcy

autor

Janeczek Janusz

• University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland

autor

Szopa Krzysztof

• University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland

autor

Fabiańska Monika

• University of Silesia, Institute of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland

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Uwagi

Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).