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)
Authors
Zdzisław Adamczyk
Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology Akademicka 2 Street, 44-100 Gliwice
Joanna Komorek
Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology Akademicka 2 Street, 44-100 Gliwice
Jacek Nowak
Silesian University of Technology, Faculty of Mining, Safety Engineering and Industrial Automation, Department of Applied Geology Akademicka 2 Street, 44-100 Gliwice
Małgorzata Lewandowska
Silesian University of Technology, Planning, Financial Analyses and Controlling Office, Akademicka 2 Street, 44-100 Gliwice
Keywords:
Rare earth elements and yttrium (REY), Neogene basaltoid intrusion, Upper Silesian Coal Basin (USCB)
Abstract
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.
