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Historia Oddziału Górnośląskiego Polskiego Towarzystwa Geologicznego

Labus Małgorzata, Sikora Rafał, Strzemińska Katarzyna

Przegląd Geologiczny

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2022

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Vol. 70, nr 4

319--325

EN

The Upper Silesian Branch of the Polish Geological Society (PGS) was established in 1962 as one of the first regional branches of the PGS. Due to the specificity of the region, geologists working in Upper Silesia were most often concerned with the exploration and exploitation of hard coal in the USCB, but also undertook research on the geology of the USCB margin, polymetallic deposits, hydrocarbons, hydrogeology, and environmental protection in areas of mining activities. These problems were expressed in the topics of PGS annual meetings, field sessions and seminars. During the 60 years of activity, five PGS meetings were organized, the topics of which concerned the latest achievements in geology in the region. Already in the first years of operation of the Upper Silesian Branch of PGS, it was noticed that a special feature of this branch is the considerable dispersion of geologists working in various cities of the voivodeship. However, despite the difficulties resulting from this fact, the Upper Silesian Branch is active and it has been consolidating the scattered community of geologists in the region of Upper Silesia since its establishment.

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Oddział Górnośląski PIG-PIB jako przykład oddziału regionalnego

Zdanowski Albin

Przegląd Górniczy

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2019

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T. 75, nr 5

36--42

PL

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy w Warszawie działa na obszarze całej Polski mając do dyspozycji sześć oddziałów, dziewięć magazynów rdzeni wiertniczych i materiałów archiwalnych. Przykładem oddziału jest opisany w artykule Oddział Górnośląski (OG) w Sosnowcu działający od 1921 do 1932 roku w Dąbrowie Górniczej, a następnie przez kilka lat w Czeladzi, od 1961 w Sosnowcu. Z racji swojej lokalizacji oraz wiodącej tematyki badawczej w OG prowadzono kompleksowe badania geologiczno-złożowe, hydrogeologiczne, stratygraficzne i petrograficzne Górnośląskiego Zagłębia Węglowego i jego najbliższego otoczenia oraz Lubelskiego Zagłębia Węglowego. Począwszy od 1990 r. w zakres obowiązków OG wprowadzono ocenę złożową metanu jako kopaliny towarzyszącej oraz kartografię geośrodowiskową i hydrogeologiczną. Aktualnie prowadzone są badania doświadczalne w zakresie odmetanowania pokładów węgla przed eksploatacją górniczą.

EN

Polish Geological Institute – National Research Institute based in Warsaw operates in entire Poland, having six branches and nine core repositories and archival materials. A characteristic example is the Upper Silesian Branch (USB) in Sosnowiec that started its activities in Dąbrowa Górnicza (1921-1939), and the continued them in Czeladź (1945-1960); since 1961 the branch seat is Sosnowiec. Because of its location, the branch was concentrated on comprehensive hydrogeological, stratigraphical and petrographical research and first of all on economic-geological studies of the Upper Silesia Coal Basin and its neighbourhood as well as of the Lublin Coal Basin. Starting from 1990, the USB tasks include also the estimation of deposit potential of methane as accompanying mineral and geoenvironmental and hydrogeological mapping. Actually, experimental studies on methane drainage of coal beds prior to mining exploitation are conducted.

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Badania geologiczne Lubelskiego Zagłębia Węglowego w Oddziale Górnśląskim Państwowego Instytutu Geologicznego

Zdanowski Albin

Przegląd Geologiczny

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2019

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Vol. 67, nr 8

645--652

EN

This paper presents a brief description ofgeological surveying conducted between 1920 and 1939 in the Western Volhynian area by Professor Jan Samsonowicz who discovered Carboniferous deposits with bituminous coal beds. After the Second World War, the Geological Institute proposed a deep-hole project which was aimed at the exploration of the geological setting of Poland. In this connection, a few boreholes were drilled throughout the Lublin Voivodeship area, resulting in identification of Carboniferous deposits with bituminous coal beds. In the late 50s of the 20th century, the researchers working on coal deposits and the explorer J. Porzycki were moved to the Upper Silesian Field Station in Czeladź, which was transformed into the Upper Silesian Branch of the Geological Institute in Sosnowiec. It was this place where a research team for Carboniferous deposits, including coal-bearing deposits in Lublin area, was created. A few projects for geological works were prepared with the purpose to discover coal deposits in the area between Hrubieszów and Łuków. The first monograph of Carboniferous beds in the Lublin Coal Basin was published in 1966 (Rühle, 1966). In 1967, the most potential area was indicated as well as the Łęczna and Chelm bituminous coal deposits were identified and then documented during1971-1974. Further documentation works were taken over by the coal industry while the branch in Sosnowiec continued the research at a regional level, aiming mainly at coal deposits and simultaneously started with research on aluminum ore deposits at the base of Carboniferous strata in the northeastern part of the Lublin Coal Basin. The aforementioned research team determined geological and mining conditions of coal deposit occurrences, Carboniferous deposits stratigraphy, coal and gangue petrography, lithostratigraphy, origin and sedimentation conditions of coal-bearing formation etc. The results were presented in the monograph (Dembowski, Porzycki, 1988; Zdanowski, Żakowa, 1995), geological atlas (Porzycki, 1978; Zdanowski, 1999) and numerous articles published in Poland and abroad. The research team from Sosnowiec presented their results not only at national conferences but also at International Geological Congresses, International Congresses on the Carboniferous and Permian, one of which was organized in Cracow in 1995 by the team alone. In recent years the team from the Upper Silesian Branch rejoined the process of documentation of coal deposits through cooperation with domestic and foreign companies interested in possible future coal extraction in the Lublin area.