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Tytuł:
High-temperature restite enclave as an evidence of deep seated parent magma melting of the Będkowska Valley granodirite (Silesian-Cracow area, South Poland)
Autorzy:
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/191648.pdf
Data publikacji:
2004
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Będkowska Valley granodiorite
dark micaceous enclave
restite
Opis:
In the borehole DB-5, at a depth 1370.0 m dark micaceous enclave in granodiorite from Będkowska Valley was found. A sharp contact enclave/granodiorite is observed. The transition zone is irregularly developed around the enclave studied. It is a small enclave (3 x 6 cm), discoidal in shape. The microstructure of micaceous enclave is fine-blastic; crystalloblasts of rock-forming minerals are 0.2-0.5 mm in size. This enclave consists of: Fe-biotite (56-62 vol.%), plagioclase Ca-Na (34-40 vol.%), spinel (magnetite), corundum, and sericitic pseudo- morphs after cordierite. Its mineralogical composition is different from the Będkowska Valley granodiorite, what suggests that this rock is a medium/high-temperature restite. This rock represents residuum after partial melting of granodiorite magma in deep levels of basement of the Małopolska Massif.
Źródło:
Annales Societatis Geologorum Poloniae; 2004, 74, No 1; 21-33
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Visual Strain and Lighting Preferences of VDT Users Under Different Lighting Systems
Autorzy:
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/89822.pdf
Data publikacji:
2003
Wydawca:
Centralny Instytut Ochrony Pracy
Tematy:
VDT users
lighting systems
visual fatigue
lighting preferences
system oświetlenia
zmęczenie wzroku
preferencje oświetleniowe
Opis:
Lighting influences users’ visual strain and well-being. Therefore creating lighting that ensures visual work conditions do not results in visual fatigue is a preventive activity. The aim of the study was to model different lighting systems for visual display terminal (VDT) work and to determine their influence on users’ visual strain and preferences. The results of the study showed that visual fatigue was lowest for indirect and compound lighting systems. On the other hand, in general, direct lighting realized by “dark-light” luminaires was the most preferred lighting system. Some interesting differences related to age, gender, and VDT work experience were found. On the basis of the obtained results lighting designers can be provided with some guidance.
Źródło:
International Journal of Occupational Safety and Ergonomics; 2003, 9, 4; 431-440
1080-3548
Pojawia się w:
International Journal of Occupational Safety and Ergonomics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Occupational Exposure to Solar Ultraviolet Radiation of Polish Outdoor Workers: Risk Estimation Method and Criterion
Autorzy:
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/90766.pdf
Data publikacji:
2013
Wydawca:
Centralny Instytut Ochrony Pracy
Tematy:
UVR hazard
solar UVR occupational exposure
risk assessment
risk estimation skin exposure factor
promieniowanie nadfioletowe
praca na powietrzu
ocena ryzyka zawodowego
skóra
ekspozycja zawodowa
Opis:
This paper presents occupational skin exposure to solar ultraviolet radiation (UVR) of 122 Polish outdoor workers in spring and summer. In 65% of the cases, it was significant and exceeded 10 standard erythema doses (SED) during a work shift. The results provided grounds for (a) modifying hazard assessment based on the skin exposure factor proposed by the International Commission on Non-Ionizing Radiation Protection (ICNIRP) and (b) developing a criterion of risk estimation. The modified method uses the UV index (UVI) instead of the geographical latitude and season factor. The skin exposure factor (Wes) of one is the criterion of risk estimation. Risk is low if the estimated value of Wes does not exceed one. If it does, suitable preventive measures are necessary and a corrected skin exposure factor (Wes *) is calculated to minimize its value to at least one. Risk estimated with that method was high in 67% of the cases.
Źródło:
International Journal of Occupational Safety and Ergonomics; 2013, 19, 1; 107-116
1080-3548
Pojawia się w:
International Journal of Occupational Safety and Ergonomics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Deformation structures in the gneissic exotic pebbles from the area of Wołosate (Cisna sandstone, Dukla tectonic unit, Outer Carpathians, Poland)
Autorzy:
Kania, M.
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/191901.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
gneissic exotic pebbles
foliation
metamorphism
mica fish
Bieszczady Mts.
Outer Carpathians
Polska
Opis:
Gneissic exotic pebbles from the Cisna beds (Dukla tectonic unit) in the region of Wołosate (Bieszczady Mts., Eastern Carpathians) were investigated. These exotic pebbles are from 9.5 to 13 cm in size. Basing on the structural features, the following groups of exotic pebbles were distinguished: granitic gneisses, laminated gneisses, flaser gneisses and mylonitic gneisses. Granite - granodiorite protolith was deformed in the shear zone; strain partitioning was probably an important process during deformation. The observed structures allow to determine the temperature of metamorphism as 500-550°C. The lower limit of pressure was determined basing on phengite geobarometer as 5 kbar. The nature and localization of the source area can be similar to the Bretila sequence from the Romanian Eastern Carpathians.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 1; 41-52
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Luminance of the Surround and Visual Fatigue of VDT Operators
Autorzy:
Wolska, A.
Swituta, M.
Powiązania:
https://bibliotekanauki.pl/articles/90508.pdf
Data publikacji:
1999
Wydawca:
Centralny Instytut Ochrony Pracy
Tematy:
luminance
visual fatigue
CRT screen
luminancja
zmęczenie wzroku
oświetlenie
Opis:
Luminance distribution in the visual field is considered as one of causal factors with a significant influence on visual fatigue, especially for intensive and extended Video Display Terminal (VDT) work. The aim of the study was to define visual fatigue of VDT operators for different values of surrounding luminance. Experiments were carried out in laboratory conditions under 3 lighting conditions. Only 1 lighting parameter - the luminance of the wall behind the display (surrounding luminance) - changed. Visual fatigue was measured both by a subjective evaluation of different visual complaints (asthenopic symptoms) and by objective measurements of changes in the following visual functions: accommodation, convergence, habitual horizontal phoria, critical fusional frequency (CFF), and visual acuity. The same experiments were done for CRT (Cathode Ray Tube) and LCD TFT (Liquid Crystal Display with Thin Film Transistor) screens. The results of the study have shown that there was no significant influence of the value of surrounding luminance on the asthenopic symptoms for either type of screen. A general tendency towards bigger visual complaints for LCD TFT than for CRT participants was found. An objective evaluation of visual fatigue demonstrated a tendency towards bigger changes in visual functions with an increase of surrounding luminance for both screens. Statistical analysis of the results has shown that surrounding luminance influences significantly the reduction of the accommodation amplitude (significance level < .05).
Źródło:
International Journal of Occupational Safety and Ergonomics; 1999, 5, 4; 553-580
1080-3548
Pojawia się w:
International Journal of Occupational Safety and Ergonomics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mineralogical and geochemical study of thermally altered country rocks of granodiorite intrusion in the Będkowska Valley near Kraków (S Poland)
Mineralogiczne i geochemiczne badania przeobrażonych termicznie skał otaczających intruzję granodiorytową w Dolinie Będkowskiej koło Krakowa (południowa Polska)
Autorzy:
Koszowska, E.
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/191270.pdf
Data publikacji:
2000
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
metamorphism
thermally altered
spotted hornfels
contact aureole
granodiorite
cordierite
andalusite
Opis:
Extensive zone of thermally altered sedimentary rocks occurring in the contact aureole of granodiorite intrusion has been described from the boreholes in the Będkowska Valley near Kraków. Depending on the composition of primary rocks and the distance from the intrusion the following metamorphic rocks were formed: fine-grained cordierite hornfelses, macroscopically spotted andalusite hornfelses, chlorite-bearing spotted rocks, metaconglomerates, metasandstones and metamudstones. These rocks consist of various neogenic minerals: cordierite, andalusite, biotite, muscovite, feldspars and corundum. The rocks and neogenic minerals have been investigated in details using optical and electron microscopy, X-ray diffraction, EDS and chemical methods (ICP, INAA, XRF). Characteristic contact metamorphic mineral paragenesis suggests that the most altered rocks in question were formed within temperature range from 580 to 630°C and pressure about 1-2 kbar under conditions corresponding to the orthoclase-cordierite hornfels facies of thermal metamorphism.
Rozległa strefa przeobrażonych termicznie skał osadowych tworzących aureolę kontaktową dookoła intruzji granodiorytu została opisana z wierceń (otwory DB-5 i WB-102A) usytuowanych w Dolinie Będkowskiej (na północny zachód od Krakowa). W zależności od odległości od intruzji oraz pierwotnego składu mineralnego i chemicznego skał osadowych, podczas metamorfizmu kontaktowego powstały następujące skały: drobnoziarniste hornfelsy kordierytowe, makroskopowo plamiste hornfelsy andaluzytowe, skały plamiste z chlorytem, metazlepieńce, metapiaskowce i metamułowce. W badanych skałach stwierdzono występowanie następujących neogenicznych minerałów: kordierytu, andaluzytu, biotytu, muskowitu, skaleni i korundu. Skały przeobrażone termicznie, oraz ich neogeniczne minerały zostały szczegółowo przebadane mikroskopowo (mikroskop polaryzacyjny i elektronowy), metodą rentgenowską oraz metodami chemicznymi (klasyczna analiza chemiczna, ICP, INAA, XRF oraz EDS i mikrosonda). Obecność w badanych skałach paragenez mineralnych charakterystycznych dla facji ortoklazowo-kordierytowo-hornfelsowej metamorfizmu kontaktowego (według terminologii Winklera) może sugerować zakres temperatur (580-630°C) i ciśnień (1-2 kbar), w którym doszło do najintensywniejszej termicznej transformacji skał osadowych.
Źródło:
Annales Societatis Geologorum Poloniae; 2000, 70, No. 3-4; 261-281
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Deformation structures in the gneissic exotic pebbles from the area of Wołosate (Cisna sandstone, Dukla tectonic unit, Outer Carpathians, Poland)
Autorzy:
Kania, M.
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/191383.pdf
Data publikacji:
2009
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
gneissic exotic pebbles
foliation
metamorphism
mica fish
Bieszczady Mts.
Outer Carpathians
Polska
Opis:
Gneissic exotic pebbles from the Cisna beds (Dukla tectonic unit) in the region of Wołosate (Biesz- czady Mts., Eastern Carpathians) were investigated. These exotic pebbles are from 9.5 to 13 cm in size. Basing on the structural features, the following groups of exotic pebbles were distinguished: granitic gneisses, laminated gneisses, flaser gneisses and mylonitic gneisses. Granite - granodiorite protolith was deformed in the shear zone; strain partitioning was probably an important process during deformation. The observed structures allow to determine the temperature of metamorphism as 500-550°C. The lower limit of pressure was determined basing on phengite geobarometer as 5 kbar. The nature and localization of the source area can be similar to the Bretila sequence from the Romanian Eastern Carpathians.
Źródło:
Annales Societatis Geologorum Poloniae; 2009, 79, No 2; 41-52
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Siliciclastic input into Upper Cenomanian synorogenic sediments of the High-Tatric Unit, Central Western Carpathians (Tatra Mountains); petrography, geochemistry and provenance
Autorzy:
Wolska, A.
Bąk, K.
Bąk, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060546.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
petrography
geochemistry
Upper Cenomanian
Zabijak Formation
High-Tatric Unit
Central Western Carpathians
Opis:
The Upper Cenomanian mixed siliciclastic-carbonate succession of the High-Tatric Unit was deposited during the initial stage of basinal closing of the Tatric area, part of the Zliechov (Križna) Basin (Inner Carpathian domain). As a result of tectonic activity taking place at the northern Veporic margin, pulses of siliciclastic input interrupted marine carbonate sedimentation. The siliciclastic material, part of the Zabijak Formation, has been studied along two sections (Pisana Gully and Zdziarski Gully) in the Western Tatra Mountains. Microfacies, petrographic and geochemical analyses reveal a variability of siliciclastic material composed of various types of granitoids and medium- or high-grade metamorphic rocks, with schists and gneisses. Such interpretation is confirmed by the results of elemental chemical analyses, in which immobile trace elements, such as REE, Th, Cr, Co, Zr, and Y were used as indices for sediment provenance. The parent rocks sustained moderate to intense chemical weathering, documented by chemical weathering indices (CIA, PIA, CIW, R). The weathering occurred in a humid climate with relatively high precipitation that caused strong leaching of particles. Chemical indices related to sorting processes suggest that the recycling of the source material was a minor significance. The siliciclastic input displays a waning upward tendency in the sections, which can be associated with diminishing of the source area by gradual inland progradation of a carbonate platform, caused by a global sea level rise during the Late Cenomanian.
Źródło:
Geological Quarterly; 2016, 60, 4; 919--934
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotouristic values of the Chochołowska Valley (Tatra Mountains, Poland) and their accessibility for people with physical disabilities
Dostępność walorów geoturystycznych Doliny Chochołowskiej (Tatry, Polska) dla osób niepełnosprawnych ruchowo
Autorzy:
Chrobak, A.
Ciurej, A.
Wolska, A.
Kowalik, S.
Powiązania:
https://bibliotekanauki.pl/articles/128452.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Tatra Mountains
Chochołowska Valley
geotourism
geosites
sedimentary rocks
tourism for people with physical disabilities
Tatry
Dolina Chochołowska
geoturystyka
geostanowiska
skały osadowe
turystyka dla osób niepełnosprawnych ruchowo
Opis:
The purpose of this contribution is to present the geotourist path in the Chochołowska Valley for the disabled with limited mobility, as well as for the elderly. The Chochołowska Valley is the most westward valley in the Polish Tatra Mountains (Western Tatras). It is the longest and largest valley in the Polish Tatra Mountains, with an area of 35 km2 and 10 km in length. The highest peak located in the Chochołowska Valley is the Starorobociański Wierch at 2176 m a.s.l. The altitude at the end of the valley around Siwa Polana, is about 900 m a.s.l. (from 910 m a.s.l. to 920 m a.s.l.). At the Polana Huciska, where the geotoursit path ends, the altitude is about 1000 m a.s.l. The length of the path is 3.5 km, and the altitude difference over this distance is 100 meters. The Chochołowska Valley is developed in sedimentary rocks (limestones, marls, dolomites), belonging to two nappes: Choč Nappe (e.g. Siwiańskie Turnie outcrop) and Križna Nappe (e.g. Niżna Brama Chochołowska Rock Gate). The valley administratively belongs to the Witów village. A green tourist trail was marked through the valley. It start from the Siwa Polana to the mountain hut named after John Paul II on Polana Chochołowska. An asphalt road is from Siwa Polana to the Polana Huciska. The Chochołowska Valley is one of the most beautiful Tatra valleys with numerous rock outcrops and is considered to have a high geotouristic potential. The proposed geotourist path includes selected outcrops, which can be easily accessed by people with limited mobility, including people in wheelchairs. This path runs along a wide asphalt road, and any additional equipment (e.g. a freewheel for wheelchairs) is not required. A large car parking lot is available at the beginning of the proposed path (Siwa Polana), as well as sanitary and catering facilities.
W niniejszym artykule została opisana propozycja trasy geoturystycznej w Dolinie Chochołowskiej dla osób niepełnosprawnych z ograniczonym stopniem poruszania się oraz dla osób starszych. Dolina Chochołowska jest najbardziej na zachód wysuniętą doliną walną w Tatrach Polskich (Tatry Zachodnie). Jest to najdłuższa i największa dolina w Tatrach Polskich. Jej powierzchnia wynosi 35 km2, a długość 10 km. Najwyższym szczytem położonym nad Doliną Chochołowską jest Starorobociański Wierch (2176 m n.p.m.). Wysokość bezwzględna u wylotu doliny, w rejonie Siwej Polany, wynosi około 900 m n.p.m. (od 910 m n.p.m. do 920 m n.p.m.), a na Polanie Huciska około 1000 m n. p. m. Długość naszej ścieżki geoturystycznej wynosi 3,5 km, a różnica wysokości na tej odległości wynosi 100 metrów. Dolina Chochołowska jest wypreparowana w skałach osadowych (wapienie, margle, dolomity) dwóch płaszczowin: choczańskiej (Siwiań- skie Turnie) i kriżniańskiej (Niżna Brama Chochołowska). Dolina ta administracyjnie należy do wsi Witów. Dnem doliny został popro- wadzony zielony szlak turystyczny do górskiego schroniska im. Jana Pawła II na Polanie Chochołowskiej. Do połowy doliny, do Polany Huciska, została doprowadzona droga asfaltowa. Dolina Chochołowska jest jedną z piękniejszych dolin tatrzańskich o wysokim potencjale geoturystycznym w związku ze znajdującymi się tu licznymi odsłonięciami skalnymi. W niniejszym artykule prezentujemy wybrane odsłonięcia łatwo dostępne, do których mogą dostać się bezproblemowo (płaska i szeroka nawierzchnia drogi) osoby z ograniczonym stopniem poruszania się, w tym również na wózkach inwalidzkich. Proponowana ścieżka geoturystyczna przebiega opisywaną drogą asfaltową, co nie wymaga konieczności używania dodatkowych sprzętów (np. freewheel w przypadku wózków). Na początku proponowanej trasy (Siwa Polana) jest duży parking dla samochodów i niezbędna infrastruktura sanitarno-gastronomiczna.
Źródło:
Geotourism / Geoturystyka; 2018, 1-2 (52-53); I-XII
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geology of the Magura Nappe in the Osielec area with emphasis on an Eocene olistostrome with metabasite olistoliths (Outer Carpathians, Poland)
Autorzy:
Cieszkowski, M.
Kysiak, T.
Szczęch, M.
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/191808.pdf
Data publikacji:
2017
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Magura Nappe
Rača Subunit
Late Cretaceous-Palaeogene
lithostratigraphy
tectonics
olisto- strome
olistoliths
metabasite
Opis:
The Magura Nappe in the Polish sector of the Outer Carpathians consists of four tectonic subunits characterized by differing development of facies. From the south to the north, they include the Siary, Rača, Bystrica and Krynica subunits. The sedimentary succession in the Rača Subunit in the vicinity of the village of Osielec is composed of Campanian–Palaeogene flysch deposited in the Magura Basin. In this succession, the Middle Eocene Pasierbiec Sandstone Fm consists of thick-bedded sandstones and conglomerates with occasional intercalations of thin-bedded shale-sandstone flysch. Within the Pasierbiec Sandstone Fm at Osielec there is an olistostrome, rich in pebbles and cobbles of exotic rocks. In addition, large blocks of Neoproterozoic metabasites and boulders of Palaeogene organogenic limestones were found. The discovery of metabasites raised the possibility that the rocks in question could be evidence of supposed oceanic crust in the basement of the Magura sedimentary basin, because of the suggestion that they represent the Alpine orogenic cycle. This concept was abandoned when investigations of the absolute age of the metabasites gave a date of ca. 600 Ma. In the Osielec area, there are two tectonic thrust sheets in the Rača Subunit, namely the Osielczyk Thrust Sheet in the north and the Bystra Thrust Sheet in the south; they are folded and cut by a transverse system of strike-slip and oblique faults. The Osielczyk Thrust Sheet was overthrust northwards on to the Siary Subunit.
Źródło:
Annales Societatis Geologorum Poloniae; 2017, 87, 2; 169-182
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Practical Application of Ergonomic Settings of Typical Computerised Workstations
Autorzy:
Tokarski, T.
Liu, D.
Kamińska, J.
Wolska, A.
Powiązania:
https://bibliotekanauki.pl/articles/91119.pdf
Data publikacji:
2000
Wydawca:
Centralny Instytut Ochrony Pracy
Tematy:
computerised workstations
ergonomic settings
lighting
ergonomia
komputerowe stanowisko pracy
oświetlenie
Opis:
The goal of the study was to check, with regard to ergonomics, workstations equipped with visual display terminals in selected enterprises. Over 180 workstations were tested in 3 enterprises. Most workstations were equipped with computers. The ergonomics of both the parameters of the basic components of the workstation (i.e., a chair and a desk, and the position of the computer at the workstation and its screen with respect to windows) and lighting fittings were analysed. Typical mistakes in the layout of a workstation were chairs inappropriate for computer work, as well as broken chair adjustment mechanisms, which qualified chairs for repair or replacement. Wrong positioning of monitors on the desk and with regard to windows and lighting fittings was also noted.
Źródło:
International Journal of Occupational Safety and Ergonomics; 2000, Zeszyt Specjalny; 119-126
1080-3548
Pojawia się w:
International Journal of Occupational Safety and Ergonomics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Simulation of Reflected and Scattered Laser Radiation for Designing Laser Shields
Autorzy:
Konieczny, P.
Wolska, A.
Świderski, J.
Zając, A.
Powiązania:
https://bibliotekanauki.pl/articles/89749.pdf
Data publikacji:
2008
Wydawca:
Centralny Instytut Ochrony Pracy
Tematy:
biological and safety aspects of laser radiation
shield angle
computer simulation
measurements of reflected and scattered laser radiation
Opis:
This paper presents a computer simulation of reflected and scattered laser radiation for calculating the angle of laser shields performed with the Laser Shield Solver computer program. The authors describe a method of calculating the shield angle for laser shields which protect workers against reflected and scattered laser radiation and which are made from different materials. The main assumptions of the program, which calculates and simulates reflected laser radiation from any material and which can be used for designing shield angles, are presented. Calculations are compared with measurements of reflected laser radiation. The results for one type of laser and different materials which interacted with a laser beam showed that the Laser Shield Solver was an appropriate tool for designing laser shields and its simulations of reflected laser radiation distribution have practical use.
Źródło:
International Journal of Occupational Safety and Ergonomics; 2008, 14, 2; 133-147
1080-3548
Pojawia się w:
International Journal of Occupational Safety and Ergonomics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Coal-bearing submarine slump sediments from Oligocene–Miocene transition of the Eastern Carpathians (Bieszczady Mountains, SE Poland)
Autorzy:
Bąk, K.
Wolska, A.
Zielińska, M.
Bąk, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060286.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
coal pebbles
submarine slump
petrography
foraminifera
Oligocene–Miocene transition
Outer Carpathians
Bieszczady Mts.
Opis:
A new finding of lustrous coal particles from the youngest flysch sediments of the Silesian Nappe, Polish Eastern Carpathians, outcropped in the Bieszczady Mountains is here presented. The coal material occurs in a 1-m thick submarine slump layer in the Kiczera Dydiowska Sandstones, which belong to the youngest part of the Krosno Beds. Coal particles are numerous (up to 16%) in a massive sandstone of the slump layer. The siliciclastic particles from these sediments are classified as material from weathered rocks of continental block or they have been recycled from post-orogenic sediments. Lustrous coal represents coaly plant fragments, which are mostly homogeneous, belonging to macerals of vitrinite group. Some coal pebbles display tree structure, typical of gelified xylites, due to impregnation of cell walls by resinite, which occurrence in this material indicates terrestrial plants producing waxes and resins. Some of gelified plant debris shows evidence of pyritization, what in the absence of inertinite macerals in coal may indicate dysoxic conditions during first decomposition processes of organic matter under water environment. Coaly-bearing slump moved down most probably from SW during Oligocene–Miocene transition time. This shows that an intrabasinal massif, as the uplifted fragment of ?Precambrian craton, which supplied large amount of siliciclastic material to the Silesian–Subsilesian basin during the lower–middle Oligocene, still existed at the end of the Oligocene.
Źródło:
Geological Quarterly; 2015, 59, 2; 300--315
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Successive stages of calcitization and silicification of Cenomanian spicule-bearing turbidites based on microfacies analysis, Polish Outer Carpathians
Autorzy:
Bąk, B.
Górny, Z.
Bąk, K.
Wolska, A.
Stożek, B.
Powiązania:
https://bibliotekanauki.pl/articles/191355.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
calcitization
silicification
sponge spicules
spicule-bearing turbidites
cherts
Cenomanian
Outer Carpathians
Opis:
Mid-Cretaceous turbidites with large proportions of sponge spicules are widely distributed in the Silesian Nappe of the Outer Carpathians, giving rise to diversified types of sediments, from spiculites to spicule-bearing siliciclastics and calcarenites. Part of this succession, Middle–Late Cenomanian in age, was transformed into cherts. A microfacies study showed that these turbidite sediments underwent several stages of calcitization and silicification, which took place during Mid-Cretaceous times in different sedimentary environments, i.e., on a northern shelf bordering the Silesian Basin and on a deep sea floor. The first diagenetic changes were related to changes to the biotic components of the turbidite layers, dominated by siliceous sponge spicules. This process, which took place in the spiculitic carbonate mud on the shelves, was related to the calcitization of sponge spicules. Calcareous clasts and calcified skeletal elements also were corroded by bacteria. After transportation down the slope, the biogenic and siliciclastic particles were deposited below the carbonate compensation depth. Taphonomic processes on the basin floor and alternating phases of carbonate and silica cementations, recrystallization and dissolution occurred in these sediments and were related to the diversification in composition of successive turbidite layers. Silicification was related to the formation of quartz precipitates as fibrous chalcedony or microcrystalline quartz, which were derived from the earlier dissolution of amorphous silica, originating mostly from siliceous sponge spicules and radiolarian skeletons. However, a source of silica from hydrothermal vents was also possible. The initial silica precipitation could have taken place in a slightly acidic environment, where calcite was simultaneously dissolved. A number of silicification stages, visible as different forms of silica precipitate inside moulds after bioclasts, occur in the particular turbidite layers. They were related to changes in various elements of the pore-water profile after descending turbidity-current flows. A very low sedimentation rate during the Middle–Late Cenomanian in the Silesian Basin may have favoured the sequence of initial calcitization and silicification stages of the turbidite sediments.
Źródło:
Annales Societatis Geologorum Poloniae; 2015, 85, 1; 187-203
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
X-ray Absorption Fine Structure Investigation of the Low Temperature Grown ZnCoO Films
Autorzy:
Wolska, A.
Klepka, M.
Witkowski, B.
Witkowski, M.
Guziewicz, E.
Godlewski, M.
Powiązania:
https://bibliotekanauki.pl/articles/1431568.pdf
Data publikacji:
2012-04
Wydawca:
Polska Akademia Nauk. Instytut Fizyki PAN
Tematy:
78.70.Dm
75.50.Pp
68.55.-a
Opis:
ZnO based diluted magnetic semiconductors are intensively investigated for possible spintronic applications. In the present work we investigate the ZnCoO layers grown at low temperature by atomic layer deposition. The local atomic structure of a series of layers with different Co concentration is investigated by the X-ray absorption fine structure measurements. Two groups of ZnCoO layers are investigated - the ones with an uniform Co distribution and highly nonuniform films. For uniform samples we observe that a majority of Co atoms is built into the ZnO matrix substituting the Zn atoms. In contrast, for the nonuniform samples, metallic Co inclusions are also observed. These results are in strong correlation with the magnetic properties of the films studied separately. Samples with the uniform Co distribution (Co substitutes Zn in ZnO) are paramagnetic, whereas the nonuniform ones show a ferromagnetic response.
Źródło:
Acta Physica Polonica A; 2012, 121, 4; 883-887
0587-4246
1898-794X
Pojawia się w:
Acta Physica Polonica A
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 40

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