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    Wyświetlanie 1-9 z 9
    Tytuł:
    Report on the Polish geological investigations in the Antarctic Peninsula sector, 1987—1988
    Autorzy:
    Birkenmajer, Krzysztof
    Powiązania:
    https://bibliotekanauki.pl/articles/2053165.pdf
    Data publikacji:
    1988
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    West Antarctica
    regional geology
    stratigraphy
    tectonics
    sedimentology
    volcanology
    Źródło:
    Polish Polar Research; 1988, 9, 4; 505-519
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Report on the Polish geological investigations in West Antarctica, 1990/91
    Autorzy:
    Birkenmajer, Krzysztof
    Powiązania:
    https://bibliotekanauki.pl/articles/2052800.pdf
    Data publikacji:
    1991
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    West Antarctica
    regional geology
    stratigraphy
    sedimentology
    tectonics
    volcanology
    mapping
    Źródło:
    Polish Polar Research; 1991, 12, 3; 369-390
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Gruzja – reminiscencje z wyprawy
    Georgia – reminiscences from the expedition
    Autorzy:
    Andrusikiewicz, Wacław
    Powiązania:
    https://bibliotekanauki.pl/articles/2192068.pdf
    Data publikacji:
    2018
    Wydawca:
    Polskie Stowarzyszenie Górnictwa Solnego
    Tematy:
    wyprawa naukowa
    PSGS
    Gruzja
    geologia regionalna
    scientific expedition
    Georgia
    regional geology
    Opis:
    Gruzja, kraj pomiędzy Wielkim a Małym Kaukazem, była celem kolejnej wyprawy Polskiego Stowarzyszenia Górnictwa Solnego. Mimo że w Gruzji nie istnieje górnictwo solne jako odrębna gałąź przemysłu, to ze względu na położenie geograficzne kraj ten wydaje się być niezwykle ciekawy od strony geologicznej i krajoznawczej. Nie zabrakło jednak akcentów solnych, choć w skali mikro. W trakcie wyprawy jej uczestnicy mieli możliwość poznania niezwykle ciekawych historycznie miejsc, a także obiektów przyrody ożywionej i nieożywionej. Poznanie współczesnej Gruzji było cennym doświadczeniem i porównaniem do wielu państw wcześniej odwiedzanych w trakcie wypraw Stowarzyszenia.
    Georgia, the country between the Great and the Little Caucasus, was the goal of the next trip of the Polish Mining Association. Although there is no salt mining in Georgia as a separate branch of industry, due to its geographic location, the country seems to be extremely interesting from the geological and sightseeing side. However, there were also salt accents, although on a micro scale. During the expedition, its participants had the opportunity to learn about historically interesting places, as well as lively and inanimate nature objects. Getting to know contemporary Georgia was a valuable experience and a comparison to many countries previously visited during the expeditions of the Association.
    Źródło:
    Przegląd Solny; 2018, 14; 148--162
    2300-9349
    Pojawia się w:
    Przegląd Solny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Holy Cross Mts. area - crustal structure, geophysical data and general geology
    Autorzy:
    Dadlez, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059271.pdf
    Data publikacji:
    2001
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Holy Cross Mountains
    gravity
    deep seismic soundings
    crustal structure
    regional geology
    Opis:
    At the start of international seismic experiment CELEBRATION 2000 an attempt at the compilation of the present geophysical and geological data in the Holy Cross Mountains and their surroundings has been made. Five geological units of the first order and four their dividing fault zones have been distinguished in the area studied: uplifted part of the Precambrian Craton (A), Lublin Unit (B), Radom-Łysogóry Unit (C), Kielce-Nida Unit (D), and Upper Silesian Massif (E). They are separated by fault zones: Kock Fault Zone (1) between A and B, Kazimierz Fault Zone (2) between B and C, Holy Cross Fault (3) between C and D, Cracow-Lubliniec Fold Zone (4) between D and E. The first and last units bordering the area are not discussed in this paper. Units B and C are built on the cratonic crust up to 54 km thick. Unit C is composed of poorly correlated mosaic of crustal blocks with crust 35-45 km thick. Fault zones 1 and 3 coincide with crustal fractures while zone 2 has not its counterpart in crustal structure.
    Źródło:
    Geological Quarterly; 2001, 45, 2; 99-106
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Budowa geologiczna oraz geneza i ewolucja bloku Gorzowa
    Geology, origin and evolution of the Gorzów Block
    Autorzy:
    Karnkowski, P. H.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074804.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    geologia regionalna
    basen polski
    Polska
    geologia naftowa
    tektonika
    regional geology
    Polish Basin
    NW Poland
    petroleum geology
    tectonics
    Opis:
    From the beginning of geological investigations of the Polish Lowlands both the geological and the regional tectonic units were used simultaneously. The Szczecin-Gorzów Synclinorium should be distinguished in terms of tectono-structural rules. The Gorzów Block - as a geological unit - is defined on the basis of extent and differentiation of the Upper Cretaceous thickness or by distribution of local structures (mainly halotectonic and halokinetic ones) developed in the Zechstein-Mesozoic complex. Basement in the Gorzów Block area is uplifted in its consolidated part and also the top of Moho is elevated. Both uplifts are well correlated with the Permian-Mesozoic palaeogeothermal anomaly. The Gorzów Block incorporates also the north-western part of Wolsztyn Ridge which was active during the Permian-Mesozoic time. In the early Rotliegend time this area was characterized by volcanic activity. In the late Rotliegend it was a source for clastics deposited around the Wolsztyn Ridge. Also the carbonate platform facies of the Main Dolomite (Ca2) is associated with this uplifted area. The mentioned region is situated in the distal part of asymmetric, Polish rift basin. Development of basin analysis - as an interdisciplinary domain of the Earth Sciences - indicates the need of applying various geological units, adequate to the considering problem. Modern research methods in geology (computerization, GIS) enable the data bases creation for individual geological units necessary for study of their origin and evolution up to their present geological pattern.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 8; 680-688
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Regionalizacja tektoniczna Polski a geologiczna baza danych PITAKA
    Regional tectonic subdivision of Poland versus geological database PITAKA
    Autorzy:
    Oziembłowski, P.
    Karnkowski, P. H.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074563.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    regionalizacja tektoniczna
    geologia regionalna
    Polska
    tektonika
    stratygrafia
    baza geologiczna
    GIS
    regional subdivision
    regional geology
    Polska
    tectonics
    stratigraphy
    geological database
    Opis:
    Discussion on the tectonic regional subdivision of Poland is a good opportunity to show a range of geological information of each tectonic unit and to emphasize the necessity of improvement of geological tectonic classifications, application of which in the geological databases is essential for correct usage of data collected. A good example is a geological and geophysical database PITAKA developed in the Polish Oil and Gas Company from 1987. Actually the PITAKA database contains data from 3191 boreholes which drilled Permian and younger deposits and from 4555 boreholes pierced into the older rocks. This paper presents location of 2D and 3D seismic studies done in digital technology from its introduction in Poland in 1973. In the Polish Lowlands area the Fore-Sudetic Monocline is the best geologically recognized region. The Pomeranian Anticlinorium and the Szczecin-Gorzów Synclinorium are relatively well documented. Numerous boreholes and seismic sections in those areas are associated with intensity of exploration of raw material deposits such as hydrocarbons, coal, copper, zinc and lead, sulfur and salts. Until now the PITAKA database does not contain all drilling data from Poland but it is constantly extended and supplemented.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 10; 936-938
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Regionalizacja tektoniczna Polski-Niż Polski
    Tectonic subdivision of Poland: Polish Lowlands
    Autorzy:
    Karnkowski, P. H.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074565.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    regionalizacja tektoniczna
    geologia regionalna
    Polska
    Niż Polski
    niecka Polska
    tektonika
    podłoże
    regional subdivision
    regional geology
    Polska
    Polish Lowlands
    Polish Basin
    tectonics
    basement
    Opis:
    Presented paper is a contribution to discussion about the tectonic regionalization in Poland. The Polish Lowlands, located between the Baltic shore and the highlands of the southern and central Poland, is the area discussed here. In this region mainly the Quaternary and the Neogene deposits with thickness rarely over 300 m are exposed. On the sub-Cenozoic surface occur mainly Cretaceous, Jurassic and Triassic rocks. Structural forms of the Polish Lowlands are directly associated with the Permian-Mesozoic Polish Basin inverted at the beginning of Cenozoic time. It is worthwhile indicating here that not only the Polish Trough was inverted but also the distal part of this basin, distinguished now as the Fore-Sudetic Monocline. Subdivision of the Polish Lowlands into tectonic units on the sub-Cenozoic surface was shown on Fig. 1. In the mid-Polish area antyclinorium belts of north-west to south-east orientation are located. The basement of the Polish Basin is built of the pre-Permian deposits, tectonized during pre-Alpine phases. To analyze the geology of Poland in the sub-Permian architecture the proper tectonic map (Fig. 2) is required with only the units of first order marked. Debate on tectonics of Poland requires also a map of basement consolidation units (Fig. 3). Indispensable completion of the presented maps is a geological cross-section of the Polish Lowlands (Fig. 4). It is clear that tectonic regionalization of Poland (with special attention to the Polish Lowlands) should be demonstrated on the three basic maps here presented. Spatial (both horizontal and vertical) relations between tectonic units should be considered in the light of sedimentary basin analysis, i.e., searching processes and stages of the structural evolution which essentially contributed to the recent tectonic diversification in regional geology.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 10; 895-903
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Prace geologów Państwowego Instytutu Geologicznego za granicą
    Work abroad of geologists from the National Geological Institute
    Autorzy:
    Salski, Wojciech
    Powiązania:
    https://bibliotekanauki.pl/articles/2076082.pdf
    Data publikacji:
    2020
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    prace geologiczne za granicą
    mapowanie geologiczne
    geologia surowców mineralnych
    geochemia
    geologia regionalna
    wyprawy geologiczne
    eksperci ONZ
    Afryka
    Azja
    Ameryka Północna
    Ameryka Południowa
    geological works abroad
    geological mapping
    geology of mineral resources
    geochemistry
    regional geology
    geological expeditions
    UN experts
    Africa
    Asia
    North America
    South America
    Opis:
    Geologists of the Polish Geological Institute carried out their professional activities abroad as part of geological expeditions, in teams of several people and on individual contracts, including as experts of the United Nations. In terms of the scope of work, most of their activities were focued on research on mineral resources, mapping, geochemistry, hydrogeology and geophysics, as well as on teaching of geology at the university level. The beginnings date back to the turn of the 1950s. It began with a geological expedition to Vietnam. Mongolia was the goal of subsequent expeditions on a much wider scale. The researches were conducted from the beginning of the 1960s until the end of the 1980s. The contracts, performed in groups of several people and individually, covered about 20 countries; most of them on the African continent. They focused primarily on the search for metal ore deposits, hard coal, and chemical and rock raw materials. PGI geologists also worked as UN experts in Benin, Burundi, Chad, Gabon, Haiti, India, Madagascar, Mauritania and Niger. The results of their work on various continents were the discoveries of numerous mineral deposits and the recognition of geological structure over an area of thousands of square kilometres.
    Źródło:
    Przegląd Geologiczny; 2020, 68, 5; 437--448
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Oddział Świętokrzyski Państwowego Instytutu Geologicznego : historia, ludzie i ich dokonania naukowe
    The Holy Cross Branch of the Polish Geological Institute : history, people and their scientific achievements
    Autorzy:
    Szczepanik, Zbigniew
    Giełżecka-Mądry, Dorota
    Wieczorek, Dariusz
    Powiązania:
    https://bibliotekanauki.pl/articles/2076088.pdf
    Data publikacji:
    2020
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Państwowy Instytut Geologiczny
    Oddziały regionalne PGI
    historia geologii
    Polish Geological Institute
    PGI regional branches
    history of geology
    Opis:
    Kielce is a city situated in the centre of the Holy Cross Mountains, one of the most interesting geological areas in Europe. For this reason, institutions related to mining and geology have been operating here for over 200years. After the establishment of the Polish Geological Institute in 1919 in Warsaw, one of its founders, Jan Czarnocki, took steps to establish a regional branch of the Institute in Kielce, whose aim was to conduct scientific and exploratory research in the Holy Cross Mountains area. These activities were successfully completed in 1937, and since then, with a short break due to the Second World War, a branch of the Polish Geological Institute has been operating in Kielce. Since 1961, its headquarters have been located in a modern building, designed entirely for its needs, which has recently been modernized and expanded. Several dozen people employed in the Holy Cross Branch of the PGI-NRI carry out tasks in the field of applied geology and scientific research, focused on the study of an almost complete succession of Phanerozoic rocks in this region - from the Cambrian the history of the Holy Cross Branch of the PGI-NRI, and to present the most important to the Quaternary. The aim of this article is to provide a brief introduction to data related to the research and accomplishments of the geologists working in Kielce.
    Źródło:
    Przegląd Geologiczny; 2020, 68, 5; 404--413
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-9 z 9

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