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 "structural geology" wg kryterium: Temat

  Lista filtrów
Wyrównaj
    Wyświetlanie 1-9 z 9
    Tytuł:
    Structural development of Legoupil Formation at Cape Legoupil, Antarctic Peninsula
    Autorzy:
    Tokarski, Antoni K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2052956.pdf
    Data publikacji:
    1989
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Antarctica
    Legoupil Formation
    structural geology
    Źródło:
    Polish Polar Research; 1989, 10, 4; 587-603
    0138-0338
    2081-8262
    Pojawia się w:
    Polish Polar Research
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Insights into the palaeoenvironments, structure and stratigraphy of the lower Miocene of the Eastern Carpathians Bend Zone, Romania
    Autorzy:
    Bercea, Răzvan-Ionuţ
    Bălc, Ramona
    Tămaș, Alexandra
    Filipescu, Sorin
    Mircea Tămaș, Dan
    Guillong, Marcel
    Flavius Szekely, Flavius
    Lukács, Réka
    Powiązania:
    https://bibliotekanauki.pl/articles/22446584.pdf
    Data publikacji:
    2023
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    biostratigraphy
    tuff
    zircon U-Pb age
    sedimentology
    structural geology
    Opis:
    The ages of several Oligocene to Miocene sedimentary formations from the Eastern Carpathians Bend Zone are poorly constrained due to palaeoenvironmental factors, reworking of fossils, structural complexity and limited exposure. To help overcome these issues, this study integrates calcareous nannoplankton and foraminifera biostratigraphy with isotopic age dating (U-Pb) of volcaniclastic zircons, and sedimentological and structural observations/interpretations. Our study was carried out along an ~6-km-long section made from a series of outcrops along the Bizdidel River which exposes several formations such as the Pucioasa, Fusaru, Vinețișu, Starchiojd and Slon. We show that the Fusaru Formation consists of coarse-grained rocks deposited as confined longitudinal channel successions that migrated laterally. It is bounded by the mud-rich Pucioasa and Vinețișu formations which are lateral equivalents of the Fusaru confined channels deposited as levee/overbank units. These genetically related formations appear to reach younger ages – of the lower to middle Burdigalian based on calcareous nannoplankton and foraminifera biostratigraphy – than previously thought (upper Oligocene to lower Burdigalian). The dominant organic-rich mudstones of the Starchiojd Formation represent pelagites/hemipelagites deposited in anoxic conditions. Their middle Burdigalian age is established by a 17.41 ±0.27 Ma zircon U-Pb age of zircons from the Bătrâni Tuff in the Starchiojd Formation. Based on the similar phenocryst content, zircon U-Pb age and zircon trace element composition, the source of the tuff is suggested to be the 17.3 Ma Eger ignimbrite-forming eruption, which has proximal, near-caldera deposits in the Bükkalja Volcanic Field, Hungary. The mud-rich Slon Formation seems to be related to shelf edge/upslope failure that formed cohesive debrite avalanches resulting from foreland propagation of compression. The Slon Formation extends in this area to at least the upper part of the lower Miocene to middle Miocene. These results highlight the need to revise ages of those parts of the sequence which are poorly constrained or different in other parts of the Carpathian Basin. Such revised ages help to better constrain the understanding of the deformation history of the Carpathians.
    Źródło:
    Geological Quarterly; 2023, 67, 1; art. no. 2
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Structural control on the initiation and development of the Biała Wisełka Landslide Complex (Silesian Beskid, Outer Carpathians, Southern Poland)
    Autorzy:
    Sikora, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/184722.pdf
    Data publikacji:
    2018
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    landslides
    structural geology
    lineaments analysis
    LiDAR
    Silesian Nappe
    flysch Carpathians
    Opis:
    The numerous landslides which have developed in the mostly Cretaceous to Eocene turbiditic rocks of the Silesian Beskid are genetically and geometrically controlled by bedrock structural features, the Biała Wisełka Landslide Complex being no exception. Its location is in the headwater area of the Wisła River, on the slopes of Mt. Barania Góra (1220 m a.s.l.). The bedrock is represented by flysch strata of the Silesian Nappe (Outer Carpathian Fold-and-Thrust Belt), or, more specifically, the Upper Cretaceous turbiditic Upper Godula and Lower Istebna Beds of the Godula Thrust Sheet. The research work consisted in their mapping and structural analysis, facilitated by the use of a high-resolution digital elevation model based on LiDAR data. A comparative analysis enabled the determination of the relationships between landslides and the bedrock structure. The study results point to significant roles being played by the joint network, fault systems, the structural arrangement and the lithology of rock strata in the initiation and evolution of the studied landslide complex. An additional result of the methods applied methods was the identification and characterization of previously unknown fault zones in the study area.
    Źródło:
    Geology, Geophysics and Environment; 2018, 44, 1; 31-48
    2299-8004
    2353-0790
    Pojawia się w:
    Geology, Geophysics and Environment
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Development of fault pattern in the Silesian Nappe: Eastern Outer Carpathians, Poland
    Autorzy:
    Rubinkiewicz, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059434.pdf
    Data publikacji:
    2000
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Polish Eastern Outer Carpathians
    flysch
    structural geology
    fault slip analysis
    Opis:
    The development of fault pattern in the Silesian Nappe (Central Carpathian Depression) in the eastern part of Polish Outer Carpathians is outlined, from field observations and interpretation of air photos and radar images. Fault slip analysis and palaeostress reconstruction was applied to determine different systems of strike-slip, reverse and normal faults and the relative age of each system was determined. The results show a consistent evolution of fault systems which occurred as several episodes. Some of these episodes are local but others represent a regional pattern of faulting across the whole Polish Eastern Outer Carpathians. The beginning of fault evolution took place in Late Oligocene to Late Miocene times. The oldest phase is represented by reverse and thrust faults of system R1 with SW-NE compression; a younger phase involves origination of strike-slip faults belonging to system S1 (with the same direction of compression). Reverse (system R2) and strike-slip (system S2) faults were formed locally during a N-S compressional event. Dextral strike-slip faults of system S3 with simultanous opening of a dextral set of fault system S1 originated subsequently. The youngest events are represented by normal faults N1, N2, and N3 systems during NW-SE, and SW-NE to N-S extension.
    Źródło:
    Geological Quarterly; 2000, 44, 4; 391-403
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Fault network in Rio Colca valley between Maca and Pinchollo, Central Andes, southern Peru
    Autorzy:
    Żaba, J.
    Małolepszy, Z.
    Gaidzik, K.
    Ciesielczuk, J.
    Paulo, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/191912.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    tectonics
    structural geology
    fault activity
    Rio Colca Valley
    Andes
    southern Peru
    Opis:
    The network of faults and joints within the Mesozoic, Miocene and Pleistocene–Holocene formations was studied in the Rio Colca valley, in the Pinchollo–Lari–Maca area (Central Andes, southern Peru). A complex, multi-phase development of these structures was revealed. The results show that the structural framework of the Rio Colca valley consists of WNW–ESE and NE–SW faults, and a few W–E faults. The strike of the most common fault sets is approximately parallel (longitudinal) or perpendicular (transverse) to the W–E oriented strike of stratification surfaces in the Mesozoic sedimentary series and the W–E fold macro-structures, developed in these strata. Diagonal faults and joints are less common, although at some localities they are numerous. The recurrence of major fault systems throughout the Mesozoic and Miocene series and the Pleistocene–Holocene (mainly colluvial) deposits is proof of recent, tectonic activity in the study area. The recent faulting has led to the development of a system of distinct, primary fault scarps, tectonic grabens and horsts, as well as open fissures, which are well marked in the surface morphology, and in many cases have not yet been eroded.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 3; 279--290
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Miocene transpression effects at the boundary of Central Carpathian Paleogene Basin and Pieniny Klippen Belt - examples from Polish-Slovakian borderland
    Autorzy:
    Ludwiniak, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/184548.pdf
    Data publikacji:
    2018
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    structural geology
    tectonics
    Western Central Carpathians
    Podhale basin
    Spišska Magura
    faults
    folds
    joints
    calcite veins
    Opis:
    A geological structural study has been conducted along the tectonic contact zone of the Central Carpathian Paleogene Basin (CCPB) and Pieniny Klippen Belt (PKB) in the eastern Podhale and western Spišska Magura areas. It concerned mostly the Central Carpathian Paleogene flysch strata and, to a lesser degree, the Upper Cretaceous rocks of the PKB. Tectonic deformation structures genetically related to the important tectonic boundary in question occur within a c. 1.5–2 km-wide strip of the Paleogene flysch rocks adjacent from the south to the PKB. Two parallel structural domains have been distinguished within this strip: the contact zone proper in the north and the peri-Pieniny monocline in the south. Most of the minor faults documented in the Paleogene flysch bear a record of dextral motion parallel to the contact zone. Some dextral-reverse oblique slip faults of NE-SW and W-E trends have also been recognized. Discrepancies in the orientation and sense of movement on strike-slip faults in the Paleogene flysch rocks and those in marlstones of the “klippen envelope” of the PKB were encountered. They probably reflect differences in the structural history of both the adjacent rock complexes, as the Upper Cretaceous deposits of the PKB must have experienced more deformation events and, in general, were affected by much more intense strain than those of the CCPB. Contractional structures, such as south-vergent reverse faults and recumbent folds which point to ca N-S tectonic shortening, have also been found in the Paleogene rocks. The entirety of the structural features found in the CCPB is characteristic of a transpressional regime. The regionally consistent coexistence of structures resulting from strike-slip movements and tectonic shortening, as well as features pointing directly to a transpressional regime, prove the transpressional dextral nature of the contact between the CCPB and PKB.
    Źródło:
    Geology, Geophysics and Environment; 2018, 44, 1; 91-100
    2299-8004
    2353-0790
    Pojawia się w:
    Geology, Geophysics and Environment
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    What are cleats? Preliminary studies from the Konin lignite mine, Miocene of central Poland
    Autorzy:
    Widera, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/94350.pdf
    Data publikacji:
    2014
    Wydawca:
    Uniwersytet im. Adama Mickiewicza w Poznaniu
    Tematy:
    lignite cleats
    structural geology
    lignite seams
    Miocene
    Central Poland
    węgiel brunatny
    geologia strukturalna
    pokłady węgla brunatnego
    miocen
    Polska centralna
    Opis:
    Cleats (fractures, joints) are discontinuities in coals, including lignites. They are important in mining activity because of their gas and water permeability in hard coal, and mainly because of their water permeability in lignites. As opposed to hard-coal cleats, lignite cleats have not been studied in detail before. The present contribution does so, using as an example the 1st Middle-Polish Lignite Seam (MPLS-1) in the Jóźwin IIB opencast mine in central Poland. It should be mentioned here that any remarks in the present contribution concerning MPLS-1 refer exclusively to this lignite seam in the Jóźwin IIB opencast mine. The investigated discontinuities consist of two sets, i.e. the face and butt cleats, which are roughly oriented NW–SE and NE–SW, respectively. The mean spacing of the face cleats is ~12.4 cm, while the mean spacing of the butt cleats is ~12.8 cm. The maximum average aperture is ~4.9 mm for the face cleats and ~4.1 mm for the butt cleats. The cleat spacing and aperture do not depend on the lignite thickness, but the cleat spacing increases with increasing mineral-matter and xylite content, whereas the aperture increases when the contents decrease. The regional folding and local salt diapirism tentatively explain the formation of the orthogonal system of the lignite cleats, partly because of the parallelism of the face cleats and the major tectonic directions in central Poland.
    Źródło:
    Geologos; 2014, 20, 1; 3-12
    1426-8981
    2080-6574
    Pojawia się w:
    Geologos
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Udostępnione pogórnicze obiekty podziemne Dolnego Śląska jako zaplecze geoturystyczne
    Underground tourist routes of Lower Silesia as geotourist objects
    Autorzy:
    Zagożdżon, P. P.
    Zagożdżon, K. D.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075015.pdf
    Data publikacji:
    2013
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    geotourism
    underground tourist routes
    Lower Silesia
    petrography
    mineralogy
    structural geology
    mining
    geoturystyka
    pogórnicze obiekty podziemne
    Dolny Śląsk
    petrografia
    mineralogia
    geologia strukturalna
    górnictwo
    geologia str
    Opis:
    Tourist routes in the historic underground mining workings are an ideal base for geotourism. Lower Silesia is an area favoured in this respect, due to the amount and variety of such objects. They allow observation of different geological units: diversity of their lithology, mineralization, types of deposits, tectonics, as well as very interesting aspects of mining. This paper presents proposals of geotourist routes or observation sites in underground facilities described for Złoty Stok, Krobica, Kowary, Kletno and Osówka. Long and continuous lithological profiles, interesting rocks (e.g. rheomorphic granites in Osówka), signs of mineralization (löllingite in Złoty Stok, fluorite and amethyst in Kletno), numerous dislocation zones and folds, well-preserved historic mining workings (16th and 18th- century adits in Krobica) and many others are available for observation in these objects.
    Źródło:
    Przegląd Geologiczny; 2013, 61, 1; 19--24
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Powierzchnie strukturalne w górotworze złóż węgla brunatnego, ich charakterystyka i właściwości fizyko-mechaniczne
    Structural surfaces in the overburden soils of the lignite deposits, their characteristic and geotechnical properties
    Autorzy:
    Kaczmarczyk, R.
    Rybicki, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/349148.pdf
    Data publikacji:
    2007
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    geologia inżynierska
    kopalnia odkrywkowa
    osuwiska
    powierzchnie strukturalne
    engineering geology
    open pit mine
    landslides
    structural surfaces
    Opis:
    Obserwacje prowadzone na terenie odkrywkowych kopalń węgla brunatnego wskazują na istnienie w górotworze pewnych charakterystycznych powierzchni, po których najczęściej dochodzi do powstawania osuwisk. Są to zazwyczaj powierzchnie osłabień strukturalnych, powstałe w wyniku procesów sedymentacyjnych, erozyjnych, tektonicznych, glacitektonicznych lub antropogenicznych. W artykule opisano typy powierzchni strukturalnych występujących w kopalniach węgla brunatnego oraz scharakteryzowano czynniki determinujące wartości oporów ścinania na powierzchniach strukturalnych.
    Field observations of geological profile of the overburden soils of lignite deposits Turów and Bełchatów shows some structural surfaces used as a slip surfaces of many landslides. They are usually surfaces of loosing structure of soil came to the existance after sedimentary, tectonic and erosion processes. In the article types of these surfaces, their structural character and some geotechnical properties are described.
    Źródło:
    Górnictwo i Geoinżynieria; 2007, 31, 3/1; 237-245
    1732-6702
    Pojawia się w:
    Górnictwo i Geoinżynieria
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-9 z 9

      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