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    Wyświetlanie 1-2 z 2
    Tytuł:
    Polskie zagłębia węgla kamiennego : przegląd informacji i badań geologicznych
    A short overview of data on geological investigation of the Polish bituminous coal basins
    Autorzy:
    Jureczka, J.
    Nowak, G. J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075528.pdf
    Data publikacji:
    2016
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Górnośląskie Zagłębie Węglowe
    Dolnośląskie Zagłębie Węglowe
    Lubelskie Zagłębie Węglowe
    warstwy węglonośne
    Upper Silesian Coal Basin
    Lower Silesian Coal Basin
    Lublin Coal Basin
    coal-bearing strata
    Opis:
    Polish bituminous coal basins are associated exclusively with Carboniferous deposits, differing in origin and geological structure. This paper presents only a short review of papers mainly of Polish authors on the geological structure, stratigraphy of coal-bearing deposits, quality of coal, as well as selected aspects of economic geology of three Polish bituminous coal basins: the Upper Silesian Coal Basin (USCB), Lower Silesian Coal Basin (LSCB) and Lublin Coal Basin (LCB). The paper provides also an overview on the investigations made on the interpretations of the origin of Polish coal deposits over the last 20 years with an emphasis on coal facies studies. The paper content is related to the conference entitled "Polish Coal” of the 3 rd Polish Geological Congress, which is planned in Wroclaw in September 2016. This conference covers a broad spectrum of issues such as: geology of coal basins and coal deposits, coal-bed methane, economic geology, petrology and geochemistry of coal, as well as origin, coalification and quality of coal.
    Źródło:
    Przegląd Geologiczny; 2016, 64, 9; 617--630
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Metoda punktowej, długookresowej satelitarnej interferometrii radarowej (PSInSARTM) w rozpoznaniu geodynamiki NE części Górnośląskiego Zagłębia Węglowego
    Permanent Scatterer Interferometry (PSInSARTM) technique for recognizing geodynamics of northeastern part of the Upper Silesian Coal Basin
    Autorzy:
    Graniczny, M.
    Czarnogórska, M.
    Kowalski, Z.
    Leśniak, A.
    Jureczka, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074595.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    satelitarna interferometria
    Górnośląskie Zagłębie Węglowe
    satellite interferometry
    subsidence
    Upper Silesian Coal Basin
    Opis:
    Polish Geological Institute as a member of TerraFirma Consortium obtained PSInSAR dataset for the Sosnowiec area (Upper Silesian Coal Basin - USCB) in mid-March 2004 and in spring 2006. The area of dataset covers northeastern part of the Upper Silesian Coal Basin. Processing of the data has covered scenes both ERS-1, ERS-2 registered between 1992 and 2006. The PSInSAR data were processed by TeleRilevamento Europa. Interpretation of the Sosnowiec scene has covered analysis of the multi-thematic data, including geostatistics, land use, mining, geology and seismicity. The most interesting results obtained in the Sosnowiec area are as follows: the indicated subsidence values in the period from 1992 to 2003 vary between-39.63 mm to +25.12 mm. These values show tendencies of the slow ground motion with a very high accuracy. Preliminary interpretation of the PSInSAR data of the Upper Silesian Coal Basin indicated strong correlation between the recorded PS negative values and structural pattern of the Carboniferous strata. Clearly visible concentration of negative values is also noted at footwalls and hanging walls of the Będzin and Kłodnica regional faults. Undoubtedly, the two mentioned faults of the Variscan origin were rejuvenated during the Alpine Orogeny (Triassic deposits were found in the hanging walls of the faults). The presence of the ground motion along its strike, can suggest neotectonic character of these faults. Linear anomalies oriented WNW-ESE were formed by changing values of the ground motions which are also parallel to the productive Carboniferous deposits forming the coal basin such as the Mudstone Series, Paralic Series and Upper Silesian Sandstone Series. The explanation of these phenomena (genesis and mechanisms) needs further studies. There is an evident correlation between linear negative anomalies and induced seismicity, mainly in the vicinity of the Kłodnica fault. Interpretation of slow ground motions registered by PSInSAR method from the USCB indicates also probably prolongation of the Będzin fault in northwest direction and subsidence of the Upper Silesian Sandstone Series compared to the Mudstone Series and Paralic Series.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 9; 826-835
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-2 z 2

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