Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

English (EN)·Polski (PL)·Yкраїнський (UK)
Przejdź do strony domowej biblioteki Centralna Biblioteka Wojskowa Link otwiera się w nowym oknie Logo biblioteki Prolib Integro - strona głównaCentralna Biblioteka Wojskowa

Wyszukujesz frazę "pas" wg kryterium: Temat

  Lista filtrów
Wyrównaj
    Wyświetlanie 1-7 z 7
    Tytuł:
    Zmiany wydajności monitorowanych źródeł w Pienińskim Parku Narodowym w latach 2003–2014 (pieniński pas skałkowy)
    Variation of springs discharge in Pieniny National Park in the years 2003–2014 (Pieniny Klippen Belt)
    Autorzy:
    Humnicki, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075386.pdf
    Data publikacji:
    2015
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    wydajność źródeł
    Pieniński Park Narodowy
    Pieniński pas skałkowy
    spring discharge
    Pieniny National Park
    Pieniny Klippen Belt
    Opis:
    The paper presents the 12-years discharge variations of the three springs located within the Pieniny National Park. The background was the observations of the water table variation in the springs and seasonal measurements of the springs discharge, which made the possibility of calculation of the rating curves. Generally, the Pieniny springs are characterized by low discharge. The mean discharge of the springs studied for the period 2003–2014 was as follows: spring of the Potok pod Wysoki Dział – 1.66 dm3s‒1, spring of the Kotłowy Potok – 0.26 dm3s‒1, seasonal spring of the Kirowy Potok – 0.10 dm3s‒1. Variations of the springs discharge are different due to the fact that particular spring drain separate, and relatively small groundwater reservoir. First of all, the influence of the many-years variation in the sum of atmospheric precipitation as well as the amount of infiltrating meltwater can be observed. Observations with monthly distribution showed the characteristic shift between maximum discharge of the spring and the sum of atmospheric precipitation (about 1 month shift) as well as the thawing period (1–3 months shift). Presumably, during dry seasons the springs have mainly the thawing regime, in the normal (balanced) seasons – the thawing-precipitation regime is dominant, and during the wet season – the precipitation-thawing regime prevails. In the years 2012 and 2013 the sudden decrease of discharge of the Kotłowy Potok and Kirowy Potok springs have been observed which is in well agreement with the hydrogeological drought identified in Poland.
    Źródło:
    Przegląd Geologiczny; 2015, 63, 10/1; 750--755
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Skały w krajobrazie obszaru Barberton (RPA) i ich potencjał geoturystyczny
    Rocks in the landscape of the Barberton area (South Africa) and their geotouristic potential
    Autorzy:
    Radwanek-Bąk, Barbara
    Bąk, Bogusław
    Powiązania:
    https://bibliotekanauki.pl/articles/20208868.pdf
    Data publikacji:
    2023
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    pas zieleńcowy Barberton
    archaik
    komatyt
    geotrasa Barberton Makhonjwa
    Barberton Greenstone Belt
    Archaic
    komatiite
    Barberton Makhonjwa Geotrail
    Opis:
    The area around the city of Barberton in the north-east part of South Africa is built of varied rocks belonging to the so-called Barberton Greenstone Belt (BGB), which are among the oldest (Paleo-and Mesoarchaic) and best preserved in the world. Their observation directly in the field is possible thanks to the “Barberton Makhonjwa Geotrail” created in 2014. The article briefly presents the geological structure of this area and provides important information on the development of the Earth in the Archaic, in the light of the latest research. Examples of representative outrops of BGB rocks and the close relationship between the geological structure and morphology are presented. The important raw materials of this area, including rich gold deposits (“Sheba”and others), known since the 19th century, are also mentioned.
    Źródło:
    Przegląd Geologiczny; 2023, 71, 1; 44-50
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Identyfikacja okresów suszy hydrogeologicznej na podstawie obserwacji źródeł w Pienińskim Parku Narodowym (pieniński pas skałkowy) – wyniki wstępne
    The identification of hydrogeological droughts based on observations of springs located in the Pieniny National Park (Pieniny Klippen Belt) - preliminary results
    Autorzy:
    Humnicki, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075656.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    monitoring źródeł
    susza hydrogeologiczna
    Pieniński Park Narodowy
    pieniński pas skałkowy
    spring monitoring
    hydrogeological drought
    Pieniny National Park
    Pieniny Klippen Belt
    Opis:
    The paper discusses the results of stationary limnimetric observations conducted since 2003 for three springs located in Pieniny Czorsztyńskie within the Pieniny National Park. Current knowledge on the hydrogeological regime of the examined springs, and especially their response to precipitation, meltwater supply and type of discharge recession during periods with no water supply indicated that all the springs drained small local groundwater reservoirs characterized by rapid water exchange. One of the springs was ofperiodic nature. Relatively short (14 years) observational series on spring discharge were used to identify the periods of low flow and hydrogeological drought. In order to achieve this goal, total precipitation and snow cover thickness were analyzed in individual hydrological years. Low flow periods were defined as those when the spring discharge dropped below an average value calculated on the minimum annual spring discharge for the observation period. Identification of the hydrological drought was based on the interpretation of moving average values, which allowed for the elimination of changes in spring discharge due to seasonal fluctuations and random deviations. The basis for the determination of hydrogeological droughts were the deviations ofmoving average values from the mean value over the entire observation period. The methodology was similar to the ways of determining hydrogeological drought described by other authors in mountainous areas of Poland. Periods of the most severe hydrogeological drought in the Pieniny occurred in the 2003-2004, at the turn of 2005 and 2006, in 2012, and in the 2015-2016. Specific dates of drought occurrence for different springs were variable and depended on the morphological location of the spring and local hydrogeological conditions.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 11/2; 1264--1269
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zastosowanie metody K-Ar do oznaczenia wieku deformacji skał metaosadowych formacji Yargait terranu Zavkhan (Khasagt, Mongolia) : wstępne wyniki badań
    K-Ar dating of deformation of metasedimentary rocks from the Yargait Formation of the Zavkhan terrane (Khasagt Mountains, Mongolia) : preliminary results
    Autorzy:
    Sikora, Rafał
    Wójcik, Antoni
    Szczerba, Marek
    Bazarnik, Jakub
    Madej, Stanisław
    Powiązania:
    https://bibliotekanauki.pl/articles/2076208.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    metoda K-Ar
    muskowit
    tektonika
    terran Zavkhan
    Mongolia
    środkowoazjatycki pas orogeniczny
    K-Ar dating
    muscovite
    tectonics
    Zavkhan terrane
    Central Asian Orogenic Belt
    Opis:
    The SW margin of the Zavkhan terrane is significant for research on Paleozoic amalgamation of the Central Asian Orogenic Belt (CAOB). The study area is located in the western part of the Khasagt Mountains, western Mongolia. We present a new preliminary K-Ar dating of metasedimentary rocks from the Yargait Formation which were deformed during collision of the Zavkhan terrane with the Lake Zone terrane. Our results include two dating that are similar to earlier data by other authors (Stípskáetal., 2010; Bold et al., 2016b). The first dating equal to 544.1 ±13.7 Ma can be interpreted as the age ofmetamorphism and the subduction of the SW margin ofthe Zavkhan terrane under the Lake Zone terrane during the late Ediacaran-early Cambrian. The second dating of 441.1 ±11.7 Ma indicates the Late Ordovician - Silurian regional extension event.
    Źródło:
    Przegląd Geologiczny; 2021, 69, 7; 448--453
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Chondryt węglisty NWA 4446
    Carbonaceous chondrite NWA 4446
    Autorzy:
    Przylibski, Tadeusz A.
    Blutstein, Konrad
    Łuszczek, Katarzyna
    Gruchot, Joanna
    Powiązania:
    https://bibliotekanauki.pl/articles/2087069.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    meteoryt
    chondryt węglowy
    chondryt CV3
    Asteroida typu C
    pas asteroid
    Układ Słoneczny
    ruda
    meteorite
    carbonaceous chondrite
    CV3 chondrite
    C-type asteroid
    asteroid belt
    Solar System
    ore mineral
    Opis:
    The authors carried out petrographic, mineralogical, and chemical analyses (bulk chemical composition and microanalyses of mineral chemical composition) of NWA 4446 carbonaceous chondrite. NWA 4446 chondrite is classified as CV3, S2, W2. This meteorite is a rock fragment most likely from one of the C-type asteroids orbiting the Sun in the outer part of the asteroid belt. It represents the matter formed at the earliest stages of the formation of extrasola bodies in the solar system. As a result of the research, the authors documented a wider range of variation in the chemical composition of olivine crystals (Fa: 0.67-46.57 mol%) in the matrix and chondrules, and a much narrower range of variation in the chemical com- position of pyroxene crystals (Fs: 0.90–3.35 mol%) against the data used for the classification of the meteorite. The characteristics of the chondrules, ranging in size from 0.5 to more than 1 mm, allowed concluding that they constitute about 60% of the meteorite’s vol- ume, in which they form many structural and mineral varieties PO, POP, BO, PP and RP chondrules were observed. The remaining 40% of the chondrite volume is a matrix consisting of small crystals of pyroxenes, olivines, glass, as well as opaque minerals: sulphides, FeNi alloy, native copper and gold grains, carbonaceous substance, and compact CAIs. The mineral and chemical composi- tion of CAIs shows that their dominant mineral is melilite, accompanied by diopside and spinel. The chemical composition of spinel and diopside is very similar to their total chemical formulas, while the composition of melilite shows a significant sodium deficiency. Among the opaque minerals, one phase of the FeNi dominates - awaruite (Ni 3 Fe), and sulphides are represented by troilite (FeS) and mackinawite ((Fe,Ni) 9 S 8 ). Moreover, grains of native copper with an admixture of gold and grains of native gold with an admixture of platinum, nickel and copper with a size of several μm were identified. Taking into account the admixtures contained in the above-mentioned opaque minerals (mainly Co and Cu), the parent rock of the carbonaceous chondrite NWA 4446 can be considered to have been mineralized with Fe, Ni, Co and Cu ore minerals with the content of Au and Pt. This means that, we can expect deposits of native forms of the above-mentioned metals and sulphides on the parent bodies of carbonaceous chondrites of the CV group - C-type asteroids.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 7; 513--526
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Bolesław Bujalski – geolog o bohaterskim życiorysie
    Bolesław Bujalski – a geologist of heroic biography
    Autorzy:
    Miecznik, J. B.
    Wołkowicz, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075054.pdf
    Data publikacji:
    2013
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    geology
    Flysch Belt
    Eastern Carpathians
    oil prospecting
    First World War
    Defense of Lviv
    Stanisławów
    Second World War
    geologia
    pas fliszu
    Karpaty Wschodnie
    poszukiwania ropy
    I wojna światowa
    obrona Lwowa
    II wojna światowa
    Opis:
    Doctor Bolesław Bujalski (1888-1945) graduatedfrom Lviv University to become an outstanding Polish geologist and cartographer. His major fields of expertise included tectonics and structural geology of the Flysch Belt of the Outer Eastern and Western Carpathians and oil potential in these regions. His professional career included work for a petroleum company Towarzystwo Naftowe "Galicja" S.A. and the Polish Geological Institute. During the First World War, he served in the Austro-Hungarian army. Hefought on the Russian and Italian fronts and advanced to the rank ofLieutenant. After the war, in November 1918 Doctor Bujalski he joined the reborn Polish Army in the rank of Captain and took part in a battle called the Defense of Lviv in the Polish historiography. He also fought in the Polish-Soviet War in 1920. For his distinguished merits, he was awarded the highest military distinction of Poland, the Silver Cross of the War Order of"Virtuti Militari". During the Second World War, he headed the Relief Committee of the Central Welfare Council in Stanisławów, a charity organization operating in Poland under the German occupation. He tried to continue these activities after the entry of the Red Army into the Stanisławów area in 1944 to be soon arrested by the Soviet security services (NKVD) and die in a jail most probably in early 1945.
    Źródło:
    Przegląd Geologiczny; 2013, 61, 4; 230--233
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ludwik Horwitz – badacz pienińskiego pasa skałkowego, najtrudniejszej struktury Karpat
    Ludwik Horwitz – researcher of the most difficult Carpathian structure, Pieniny Klippen Belt
    Autorzy:
    Miecznik, J. B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075148.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Maurice Lugeon Alpine School of Geology
    Polish Geological Institute in Warsaw
    geology of the Carpathians
    Pieniny Mts.
    Klippen Belt
    German occupation in Poland
    Alpejska Szkoła Geologii Maurice Lugeona
    Polski Instytut Geologiczny w Warszawie
    geologia Karpat
    Pieniny
    pas skałkowy
    niemiecka okupacja Polski
    Opis:
    Louis Horwitz (1875–1943), a Polish geologist of Jewish origin. Representative of the Alpine School of Geology of Prof. Maurice Lugeon in Lausanne. He was engaged in geological mapping in the Fribourg Alps. From 1919, he was associated with the Polish Geological Institute in Warsaw. Louis Horwitz conducted a detailed geological study of the Pieniny Klippen Belt, an orogenic suture zone between the Inner and Outer Carpathians. His research has contributed significantly to broadening knowledge of the stratigraphy of rocks composing the structure. Simultaneously, he was conducting mapping work of oil-bearing areas of the Eastern Flysch Carpathians. During the German occupation of Poland (after 1939), he continued research in the Pieniny Mts. Murdered by the Nazis in 1943.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 6; 290--294
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-7 z 7

      Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies