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 "geology" wg kryterium: Temat

  Lista filtrów
Wyrównaj
Wyświetlanie 1-15 z 135
Tytuł:
Comparison of radon hazard to inhabitants of the Augustów Plane sandr and inhabitants of the Suwałki region of fluvioglacial sands and gravels
Autorzy:
Karpińska, M.
Wołkowicz, S.
Mamont-Cieśla, K.
Mnich, Z.
Kapała, J.
Powiązania:
https://bibliotekanauki.pl/articles/148346.pdf
Data publikacji:
2003
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
building
geology
radon
Opis:
In a region of two lithologic units: the Augustów Plane sandr and the Suwałki sands and fluvioglacial gravels, 134 measurements of radon concentrations in dwelling houses were performed. An integral method of solid state nuclear trace detectors (SSNTD) was used in the studies. Statistically significant differences in the radon concentrations in both geological units were obtained. The radon concentration arithmetic mean was 197 Bq m-3, geometric mean - 119 Bq m-3, median - 111 Bq m-3, the maximal value being 1225 Bq m-3 in the region of the Suwałki fluvioglacial sands and gravels. The Augustów Plane sandr revealed arithmetic mean of radon concentration equal to 123 Bq m-3, geometric mean – 80 Bq m-3, and median equal to 67 Bq m-3, maximal value 695 Bq m-3. The annual effective dose of the radon obtained by inhabitants of the Augustów Plane sandr is 1.7 mSv and for inhabitants of the Suwałki fluvioglacial sands and gravels it is 2.5 mSv.
Źródło:
Nukleonika; 2003, 48, 4; 197-200
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka warunków geologiczno-inżynierskich podłoża Krakowa z uwzględnieniem nawarstwień historycznych
Autorzy:
Rybicki, S.
Krokoszyński, P.
Herzig, J.
Powiązania:
https://bibliotekanauki.pl/articles/343937.pdf
Data publikacji:
2007
Wydawca:
nakł. Maciej Pawlikowski
Tematy:
Kraków
geologia
geology
Źródło:
Auxiliary Sciences in Archaeology, Preservation of Relics and Environmental Engineering; 2007, T. 3 spec. ed.; 1-5
1689-6742
Pojawia się w:
Auxiliary Sciences in Archaeology, Preservation of Relics and Environmental Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geological history of the NW Indian Plate Tethyan passive margin in the Salt Range, Pakistan
Autorzy:
Iqbal, Saqib
Powiązania:
https://bibliotekanauki.pl/articles/24202115.pdf
Data publikacji:
2023
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Tethys
Pakistan
geology
Opis:
The generally east-west trending Salt Range, located in northern Pakistan, is a part of the foreland zone of the Himalayan Fold and Thrust Belt (HFTB). The 5,000–1,000 m thick Precambrian to Pleistocene sedimentary archives of the Salt Range provide an excellent opportunity for the reconstruction of sedimentation style, palaeoclimatic conditions, and tectonic history of the northwestern margin of the Indian Plate. The Precambrian evaporites of the Salt Range Formation are the oldest rocks in the area and represent the westward extension of the Precambrian evaporitic belt that includes the Hormuz Salt Basin (Iran) and Ara Salt (Arabian Plate). A highly weathered igneous body “Khewrite” occurs in the upper part of the formation and can be correlated with the volcanic record during the Ediacaran-Cambrian transition in the Arabian Plate. The clastic-dominated Lower Cambrian succession in the area is directly overlain by the Permian Tobra Formation and with a gentle angular unconformity. The poorly sorted conglomerates of the Tobra Formation indicate deposition during the Permo-Carboniferous glaciation and the irregular distribution of the Tobra and Dandot formations in the area supports their deposition during the syn-rifting phase of the Neo-Tethys opening. The overlying Upper Permian and Mesozoic strata indicate deposition on the northwestern passive margin of the Indian Plate facing the southern margin of the Neo-Tethys. This represents the drift sequence with multiple phases of passive margin rejuvenation during the Mesozoic. The drift sequence is unconformably overlain by the Paleocene Hangu Formation. Karst bauxites mark this contact and hint at exhumation and exposure in the distal part of the underthrusting plate margin. The Hangu Formation grades upward through the Lockhart Limestone into black shales of the Patala Formation supporting deepening and the possible establishment of a trench setting in the area. The presence of thick evaporites of the Bahadar Khel Salt and Jatta Gypsum in the western part of the area (Kohat Plateau) indicates a restricted lagoonal setting during the closure of the Neo-Tethys during the Eocene. The absence of the Oligocene strata hints at the uplift and exhumation of the area during the Himalayan Orogeny. The Neogene strata of the area consist of fluvial-continental detritus and represent molasse sedimentation. Thermal history modelling based on Apatite Fission Tract (AFT) data indicates three major cooling (uplift) episodes separated by two burial phases in the area. The first cooling event (ca. 520 Ma) coincides with the emplacement of the Mansehra Granite just north of the area (ca. 516 Ma) and supports exhumation correlatable with the Pan-African Orogeny. This was followed by the first burial phase (ca. 500–370 Ma) that supports Late Cambrian–Devonian sedimentation in the area. The second cooling event (ca. 300–280 Ma) coincides with the initial rifting and exhumation associated with the Neo-Tethys opening. Therefore, it appears that the Late Cambrian–Devonian strata were deposited in the Salt Range but were subsequently eroded during the exhumation induced by the Neo-Tethys opening during Permo-Carboniferous. This was followed by Neo-Tethyan passive margin deposition throughout the Mesozoic. An additional cooling episode is observable at around ca. 60 Ma and is supported by the presence of karst bauxites at the base of the Hangu Formation. Provenance analysis of the Paleocene strata suggests that detritus for the Hangu Formation was supplied from the south (Indian Plate). The overlying Patala Formation indicates the onset of sediment supply from the north and hence the uplift of the Himalayan Orogen. The overlying Kuldana Formation supports detritus supply only from the north verifying the Neo-Tethys closure by the end of Eocene. Thus the Paleogene strata represent syn-collisional deposition of the Neo-Tethys in the Salt Range. The second burial event (ca. 20–6 Ma) occurred during the Neogene in response to molasse sedimentation in the foreland of the uplifting Himalayan Orogen that was followed by the final cooling and uplift event (ca. 4 Ma) along the Salt Range Thrust. Thus the stratigraphic successions of the Salt Range provide key information regarding the reconstruction of the northwestern Neo-Tethyan margin of the Indian Plate which can help in the understanding of Neo-Tethyan tectonics in regional and global context.
Źródło:
Geotourism / Geoturystyka; 2023, 1-2 (72-73); 29--29
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evolution of the mental picture of shale reservoir completion – 3rd Shale Science Conference (Warsaw, 9–10 June 2014) : note
Autorzy:
Liana, B.
Hadro, P.
Powiązania:
https://bibliotekanauki.pl/articles/184516.pdf
Data publikacji:
2014
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
geomechanics
geophysics
geology
Opis:
The 3rd edition of ShaleScience conference held on 9–10 June 2014 in Warsaw, Poland, was a very successful event. It was organized by Orlen Upstream and partner Institutions – EGI, AGH and INIG – under the Honorary Patronage of the Polish Ministry of Environment. The conference brought together world-class specialists in fields of geology, geophysics, geomechanics, drilling, reservoir completion and environmental protection. They all contributed greatly to a better understanding of the Polish shale reservoirs of moderate quality.
Źródło:
Geology, Geophysics and Environment; 2014, 40, 3; 297-299
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geology and mining of selected energy resources in China
Autorzy:
Ćmiel, S. R.
Powiązania:
https://bibliotekanauki.pl/articles/294293.pdf
Data publikacji:
2016
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
China
geology
mining
energy resources
Opis:
The article presents geological and economic characteristics of energy resources and their mining in China. Coal basins are associated with the Palaeozoic and Mesozoic fold structures connecting crystalline massifs of the Chinese Platform. In China four coal-bearing regions are delimited: the most important economically central region (Shanxi and Ordos Basin) as well as eastern, south-western and western (Xingjian). In terms of coal resources, China ranks third, and in terms of the extraction – first in the world, producing approx. 3.65 billion t a–1. In the twenty-first century Chinese mining industry has undergone restructuring involving the liquidation of small, technologically backward mines with poor safety and profitability record. The most important onshore oil and gas basins occur in Daqing, Shengli, Nanyang, Renqiu, Karamay, Dagang and Yumen, while offshore basins are in the Yellow Sea and South China Sea. In terms of crude oil consumption and import China takes the first place in the world. Natural gas plays a relatively small role in energy production. China has the largest shale gas reserves in the world (36 trillion m3) and it is intensively preparing for their extraction.
Źródło:
Landform Analysis; 2016, 32; 3-8
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Początki badań impaktów
Beginnings of impacts research
Autorzy:
Brachaniec, Tomasz
Powiązania:
https://bibliotekanauki.pl/articles/1032957.pdf
Data publikacji:
2013
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
craters
geology
impacts
meteorites
research
Opis:
Impacts geology is a multi-disciplinary science, focus aspects of meteoritics, astronomy, petrography, geochemistry, structural geology, sedimentology and geophysics. The first studies of craters began in the 60s. Significant events in the development of this science were: the first research of the Cosmos, development of mineralogical and geochemistry analysis and important papers. Significant progress in the development of research studies reflect the number of newly discovered craters. Many aspects associated with them, such as dating, strewnfields, water impacts are still fairly problematic.
Źródło:
Acta Societatis Metheoriticae Polonorum; 2013, 4; 9-21
2080-5497
Pojawia się w:
Acta Societatis Metheoriticae Polonorum
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
„Geolog w terenie... czyli lata 20., lata 30. na archiwalnych fotografiach Profesora Zdzisława Pazdry” : wystawa w Muzeum Geologicznym im. S. J. Thugutta naWydziale Geologii Uniwersytetu Warszawskiego
"A geologist in the field... the 1920s and 1930s in archival photos of Professor Zdzisław Pazdro collection" : exhibition at the S. J. Thugutt Geological Museum of the Faculty of Geology (University of Warsaw)
Autorzy:
Barczyk, G.
Niechwedowicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075038.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geology
history of Polish geology
old photographs
geologia
historia polskiej geologii
stare fotografie
Opis:
This paper presents a collection of archival photographs taken by Zdzis³aw and Olga Pazdro. The collection was purchased by the S. J. Thugutt Geological Muzeum (Faculty of Geology, University of Warsaw). The set of vintage photographs consists of a few hundred previously unknown large-format glass plates, celluloid negatives and prints dated 1926–1939. This unique collection documents Professor's scientific fieldwork, excavations, fieldtrips and daily life scenes.
Źródło:
Przegląd Geologiczny; 2013, 61, 12; 742--745
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The dependence of relief on tectonics in the South -West Escarpment Zone of Tomaszowskie Roztocze (SE Poland)
Autorzy:
Brzezińska-Wójcik, T.
Powiązania:
https://bibliotekanauki.pl/articles/294998.pdf
Data publikacji:
2002
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
geology
geomorphology
tectonics
relief
Roztocze
Opis:
The relatively undeforrned South-West escarpment zone (SWEZ) of Roztocze, SE Poland, is marginal to the East European Platform, which is covered by a thick succession of Palaeozoic and Mesozoic rocks. Cainozoic sediments, previously much more widely distributed and largely destroyed by erosion, still fill some valleys and also crop out in the hills of the inner and outer escarpments. The escarpment zone comprises several morphological elements: an outer hill zone, inner inselbergs and a median depression zone of tectonic origin. Transverse to the escarpment, these elements are compartmentalised by transverse valleys, many of which are fault-controlled. Morphometric and geomorphological studies show that the SWEZ of Roztocze was repeatedly tectonically activated. Neotectonic redevelopment has resulted from controls in the underlying basement. Hence there are many young faults, a large number of open fault-fissures and a complex system of joints, all of which have influenced landform development in this area to a considerable degree. The main scarps have been developed along the longitudinal fault zones and, along the transverse fault zones, breach valleys. Joint systems have controlled the development of secondary relief forms. The close association of relief and various elements of the geological structure in the SWEZ of Roztocze mean that cartographic methods can reliably be employed in studies of the landforms in this area.
Źródło:
Landform Analysis; 2002, 3; 13-24
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Annual observations of radon activity concentrations in dwellings of Silesian Voivodeship
Autorzy:
Wysocka, M.
Kozłowska, B.
Dorda, J.
Kłos, B.
Chmielewska, I.
Rubin, J.
Karpińska, M.
Dohojda, M.
Powiązania:
https://bibliotekanauki.pl/articles/148558.pdf
Data publikacji:
2010
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
radon
apartment buildings
geology
seasonal changeability
Opis:
In the paper, results of year-long measurements of radon levels in dwellings on the premises of Silesian Voivodeship are presented. Track etched detectors with polymer CR-39 foils were used in the investigations. As the studied buildings were located in different regions of Silesian Voivodeship, therefore results of measurements were analysed due to possible influence of geological structure or effect of mining operations in places, where given dwellings were situated. Elevated concentrations of radon were measured mostly in dwellings located in areas, where permeable Triassic limestone and dolomite occur, as it has been predicted. On the other hand, the impact of mining activity such as disintegration of rock-body and activation of faults plays an important role, too, because it enables radon migration and its entry into buildings. Beside the analysis of seasonal variations of radon activity concentration, the impact of temperature and pressure on these fluctuations outdoor and indoor buildings has been analysed.
Źródło:
Nukleonika; 2010, 55, 3; 369-375
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Professor Piotr Roniewicz (1936-2019) In memoriam
Autorzy:
Wysocka, Anna
Głowniak, Ewa
Szulczewski, Michał
Rudowski, Stanisław
Giżejewski, Jerzy
Karnkowski, Paweł Henryk
Pieńkowski, Joanna
Pieńkowski, Grzegorz
Skompski, Stanisław
Słaby, Ewa
Kalinowska, Anna
Sawicki, Gerard
Powiązania:
https://bibliotekanauki.pl/articles/1835582.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
biography
memories
geology
biogram
wspomnienia
geologia
Opis:
Piotr Roniewicz was born in 1936 in Warsaw, however his family roots were in Stanisławów (nowadays Ivano-Frankivsk, Ukraine). He completed his university studies at the Faculty of Geology of the University of Warsaw in 1959, gaining a Master’s Degree. He began his geological career at this Faculty already as a 4th year student. In 1981-1984 he was the Vice-Dean and later in 1984-1990 – the Dean of the Faculty. Professor Roniewicz worked there until his retirement in 2006.
Źródło:
Acta Geologica Polonica; 2020, 70, 4; 435-452
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sylwetka naukowa doc. dr hab. Krystyny Kenig
Professor Krystyna Kenig – scientific achievements
Autorzy:
Morawski, W.
Powiązania:
https://bibliotekanauki.pl/articles/2062790.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Kenig Krystyna
geologia
litologia
geology
lithology
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2010, 438; 1--6
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 135

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