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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.

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Authors and Affiliations

Zdzisław Adamczyk
ORCID: ORCID
Joanna Komorek
Jacek Nowak
Małgorzata Lewandowska
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Abstract

In paper was presented a publishing history of two Lithuanian periodicals from the beginning of 19-th century — Dziennik Wileński [Vilnius Journal], published between 1805–1806 and Gazeta Literacka Wileńska [Literary Magazine of Vilnius], issued from January until December 1806. Both publishing projects were connected with the name of their editor — Gotfryd Ernest Groddeck who brought into existence the first from mentioned journals as the literary counterbalance to Dziennik which was focused mainly on science. Unfortunately, lasting year competition brought them about finish of their issuing.

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Authors and Affiliations

Jolanta Kowal

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