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The impact of a Neogene basaltoid intrusion on the distribution of rare earth elements and yttrium in Carboniferous rocks from the Sumina area, Poland (SW part of Upper Silesian Coal Basin)

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Języki publikacji
EN
Abstrakty
EN
The Neogene basaltoid intrusions found in the S-7 borehole in the Sumina area (USCB) caused transformations of the adjacent Carboniferous rocks. The mineral and chemical compositions of the basaltoides are similar to those of the Lower Silesian basaltoides. The transformations that took place in the vicinity of the intrusion were manifested in the formation of natural coke, the secondary mineralization of these rocks (calcite, chlorite, zeolites and barite) and in the specific distribution of rare earths (REY). Among REY, the light elements (LREY) had the highest share, while the heavy elements (HREY) had the lowest share. Regardless of the lithological type of the analyzed rock, with increasing distance from the intrusion, the percentage of MREY and HREY elements increases at the expense of the light elements LREY. All analyzed distribution patterns of the REYs are characterized by the occurrence of anomalies, which often show a significant correlation with the distance of sampling points from the basaltoid intrusion. The specific distribution of REYs in the vicinity of the intrusion of igneous rocks is an indication of the impact of hydrothermal solutions associated with the presence of basaltoides on the rocks closest to them located at a temperature of over 200°C
Rocznik
Strony
31--49
Opis fizyczny
Bibliogr. 37 poz., rys., tab.
Twórcy
  • Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland
  • Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland
autor
  • Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland
  • Silesian University of Technology, Planning, Financial Analyses and Controlling Office, Akademicka 2 Street, 44-100 Gliwice, Poland
Bibliografia
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  • 20. Komorek, J., Lewandowska, M. and Probierz, K. 2010. Peculiarites of petrographic composition of coking coals in southwest part of Upper Silesian Coal Basin (Poland) as a results of thermal metamorphism influence. Archive of Mining Sciences, 55, 4, 783-798
  • 21. Kokowska-Pawłowska, M. 2018. Studium mineralogiczno-geochemiczne skał współwystępujących z węglem w pokładach 405 (warstwy załęskie) i 408 (warstwy rudzkie s.s.) w Górnośląskim Zagłębiu Węglowym, 719 p. Monograph. Wydawnictwo Politechniki Śląskiej; Gliwice.
  • 22. Kwiecińska, B., Hamburg, G. and Vleeskens, J.M. 1992. Formation temperatures of natural coke in the Lower Silesian Coal Basin, Poland. Evidence from pyrite and clays by SEM-EDX. International Journal of Coal Geology, 21, 217-235.
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  • 24. Matuszewska, A., Pusz, S. and Duber, S. 2015. Evaluation of the structure of bituminous coal from Sośnica mine in the Upper Silesian Coal Basin (Poland) using reflectance indicating surface (RIS) parameters International Journal of Coal Geology, 152, 177-188.
  • 25. Probierz, K., Pozzi, M., Kuci, P. and Płachecki K. 1988. Występowanie skał intruzywnych w stropie pokładu 403/4 KWK „Morcinek” (GZW). Przegląd Górniczy, 6, 7-10.
  • 26. Probierz, K. 1989. Wpływ metamorfizmu termalnego na stopień uwęglenia i skład petrograficzny pokładów węgla w obszarze Jastrzębia (GZW) (in Polish, detailed abstract in English). Zeszyty Naukowe Politechniki Śląskiej, Górnictwo, Gliwice, 176, Monograph.
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  • 34. Smędowski, Ł., Duber, S. and Matuszewska, A. 2015. An effect of igneous intrusion on the structure, texture and microtexture of coal from the Sośnica coal mine, Upper Silesian Coal Basin, Poland. Geological Quarterly, 59, 3, 507-516.
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  • 36. Ulrych, J., Dostal, J., Adamovic, J., Jelinek, E., Spacek, P., Hegner, E. and Kadosa, B. 2011. Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic). Lithos, 123, 133-144.
  • 37. Xiao, L., Xu, Y., Mei, H., Zheng, Y., He, B. and Pirajno, F. 2004. Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume-lithosphere interaction. Earth and Planetary Science Letters, 228, 525-546.
Uwagi
PL
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020)
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-9de71739-6b6e-4383-b17f-b443c0f39686
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