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Wyszukujesz frazę "Silesian Polish" wg kryterium: Temat


Wyświetlanie 1-3 z 3
Tytuł:
Historia Oddziału Górnośląskiego Polskiego Towarzystwa Geologicznego
History of the Upper Silesian Branch of the Polish Geological Society
Autorzy:
Labus, Małgorzata
Sikora, Rafał
Strzemińska, Katarzyna
Powiązania:
https://bibliotekanauki.pl/articles/2067544.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Oddział Górnośląski PTG
historia nauk geologicznych
Polskie Towarzystwo Geologiczne
PTG
Upper Silesian Branch
history of geological science
Polish Geological Society
PGS
Opis:
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.
Źródło:
Przegląd Geologiczny; 2022, 70, 4; 319--325
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zależność między kierunkami korytarzy jaskiń pseudokrasowych a spękaniami ciosowymi w NE części Beskidu Śląskiego (Karpaty zewnętrzne)
Correlation between orientation of pseudokarst caves and joints in NE part of the Silesian Beskid Mts. (Outer Carpathians)
Autorzy:
Tomaszczyk, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074385.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
jaskinia pseudokrasowa
kierunek korytarzy
sieć spękań ciosowych
diagram
Karpaty zewnętrzne
pseudokarst caves
mass movement
joints
flysch
Godula beds
Silesian Beskid Mts.
Polish Outer Carpathians
Opis:
Numerous pseudokarst caves occur along the ridges and mountain slopes of the Silesian Beskid. These caves form in thick-bedded sandstones with dips no more than 35 , as a result of the opening of crevices present in the rock massif; this process is related to gravitational mass movements. Comparison between the direc-tions of joints and the directions of passages of fifteen selected caves shows that caves occuring in flysch rocks may form along all joint sets. The joint network of the researched area is composed of a two fold-oblique sets -Sp and SL; cross-fold set - T; and three fold-parallel sets - L, L’ and L”.
Źródło:
Przegląd Geologiczny; 2005, 53, 2; 168--174
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Historia regionalnych badań geologicznych Oddziału Dolnośląskiego PIG-PIB we Wrocławiu oraz perspektywy na najbliższe lata
History of regional geological research at the Lower Silesian Branch of the Polish Geological Institute– National Research Institute in Wrocław and prospects for the coming years
Autorzy:
Cymerman, Zbigniew
Powiązania:
https://bibliotekanauki.pl/articles/2076085.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Oddział Dolnośląski
Państwowy Instytut Geologiczny
historia badań geologicznych
mapowanie
wiercenia geologiczne
złoża minerałów
Sudety
Lower Silesian Branch
Polish Geological Institute
history of geological research
mapping
geological drillings
mineral deposits
Sudetes
Opis:
The specificity of the activities of the Lower Silesian Branch of the Polish Geological Institute - National Research Institute (PGI-NRI) is due to main factors: (1) mosaic-like geological structure of Lower Silesia, (2) the wealth of various mineral resources, (3) centuries-old mining traditions of the region. Initially, the researches included mainly geological cartography, subsequently expanding the scope of work to include regional (structural) geology and deposit geology. The contribution of applied geology, especially hydrogeology and environmental geology, has increased significantly in the previous decades. Three chapters present different periods of the Lower Silesian Branch of the PGI-NRI with its most important milestones for the Polish geology in the last seven decades. This division includes three periods: (1) years of development (1949-1989); (2) years of stagnation (1989-2013), and (3) years of disorganization (2014-2019). The period of intensification of geological researches carried out by the Lower Silesian Branch of the PGI-NRI lasted until the years of the so-called system transformation. During that period, the programs of deep boreholes were finished. In the 1990s, detailed cartographic works in Lower Silesia were completed. Acute shortage of new factographic material caused the necessity to analyze the archival material stored during previous decades at the Lower Silesian Branch. In 2014, it has practically decommissioned the regional branches, including the Lower Silesian Branch. Full centralization has led to the liquidation of both the branches’ independence and their previous focus on the implementation of tasks related to the specificity of a given region. In the forthcoming future, new challenges would depend on a proper organization chart of the PGI-NRI and the position of the regional branches in this scheme.
Źródło:
Przegląd Geologiczny; 2020, 68, 5; 378--386
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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