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Wyświetlanie 1-14 z 14
Tytuł:
Application of digital elevation models to geological and geomorphological studies - some examples
Autorzy:
Badura, J.
Przybylski, B.
Powiązania:
https://bibliotekanauki.pl/articles/2065888.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
digital elevation model (DEM)
geological cartography
SW Poland
Opis:
Analysis of the Earth’s surface using three-dimensional models provides a wealth of new interpretation opportunities to geologists and geomorphologists. Linear elements, not visible on classical maps, become distinct features; it is also possible to interpret both small-scale glacial landforms and entire complexes of postglacial landscapes at the regional scale. Geomorphic features are frequently difficult to recognise in the field, either due to their scale or field obstacles. Three-dimensional visualization of the Earth’s surface and its examination at different angles and differently orientated source of light is extremely helpful in geological and geomorphological studies. This tool is, however, relatively seldom used due to either limited access to digital data bases or time-consuming procedures of individual construction of such bases from the existing cartographic data. For instance, analysis of small-scale glacial, fluvial or aeolian landforms in lowland areas requires cartographic data of resolution compatible with 1 : 10,000 scale. Nevertheless, less detailed digital elevation models, constructed at the scale of 1 : 50,000, are also extremely helpful, since they allow for regional interpretations of those morphostructures which are associated not only with neotectonics, but also with ice-flow directions, block disintegration of an ice-sheet, subglacial drainage, stages of fluvial erosion, or location of dune belts. A possibility of superposition of geological or geomorphological maps onto 3-D models is equally important, enhancing readability of the maps and providing clues to verification of the origin of landforms and proper cross-cutting relationships drawn on the map.
Źródło:
Przegląd Geologiczny; 2005, 53, 10/2; 977-983
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmiany reżimu wydajności i potencjału zasobności źródeł : implikacje do ich klasyfikacji
Changes in discharge regime and storage capacity of the springs : implications to springs classification
Autorzy:
Buczyński, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075625.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
źródła sudeckie
współczynnik recesji
pojemność magazynowa
SW Polska
springs
recession coefficient
storage capacity
SW Poland
Opis:
The paper presents the results of precipitation influence on the discharge regime changes of 6 springs located in south-western Poland and draining a variety of rocks differing in lithology and age. Calculations for the very wet (2010) and the extremely dry years (2015) have shown that the low spring discharges experienced the greatest variations, with the coefficient ofvariation falling between 3-141%. The coefficient of variation for the maximum and average discharges generally does not exceed 90%. The obtained values of the regression coefficient from 0.0016 to 0.1 d-1 and the coefficient of variation (0-33%) indicate a relatively low variability of groundwater resources and the low transmissivity and high storage capacity of the weathering cover. The spring discharge analysis indicates also the drainage of groundwater bodies of various capacity. The maximum values of the storage capacity are several hundred thousand cubic meters, whereas in the lowest spring resources it does not exceed several thousand cubic meters. Three springs have shown a low variability of the storage capacity (Cv = 4-32%), two have indicated a moderate variability (66 and 70%) and one has shown a large variability (135%). The large storage capacity and high hydraulic resistance of the weathering cover does not guarantee the spring recharge during longer periods (summer-autumn) without rain.
Źródło:
Przegląd Geologiczny; 2017, 65, 11/2; 1179--1183
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
O konieczności wykonania drugiej edycji Szczegółowej Mapy Geologicznej Sudetów w skali 1 : 25 000 – analiza dotychczasowego stanu i założenia kompleksowej realizacji
On the need to develop the second edition of the Detailed Geological Map of the Sudetes at the scale of 1 : 25,000 - current state analysis and assumptions of a comprehensive program for the second edition
Autorzy:
Cymerman, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2075536.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Szczegółowa Mapa Geologiczna
kompleksowy projekt
Sudety
SW Polska
detailed geological mapping
comprehensive project
Sudetes
SW Poland
Opis:
Basic statutory task of the Polish Geological Institute-National Research Institute within the framework of the State Geological Survey is conducting detailed geological mapping ofPoland. One of the leading themes of the III Polish Geological Congress is the "Geological mapping - history and contemporary challenges”. The article presents an analysis of the current state ofdetailed geological mapping in the Sudetes and adjacent areas, as well as the reasons for the need to start a new, second edition of the Detailed Geological Map of the Sudetes (SMGS) at the scale of 1 : 25,000. These reasons can be briefly defined as follows: long-lasting duration of the SMGS development (nearly half a century), lack of uniformity, and outdatedness of this edition. The first edition covered 139 map sheets at the scale of1 : 25,000, with a total area over 10,100 km2. The newly presented comprehensive project assumes very fast workflow, just 10 years of work before the implementation of the second edition of the 1 : 25,000 SMGS. The new edition is going to be more modern and based on the new classification of rocks, providing more information about their origins, geotectonic settings, as well as the processes and geological phenomena, which are not included in the first edition of the 1 : 25,000 SMGS.
Źródło:
Przegląd Geologiczny; 2016, 64, 9; 604--610
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Strefy perspektywiczne występowania niekonwencjonalnych złóż węglowodorów w kambryjskich, ordowickich, sylurskich i karbońskich kompleksach skalnych Polski : integracja wyników badań
Prospective zones for unconventional hydrocarbon resources in Cambrian, Ordovician, Silurian and Carboniferous rocks of Poland : integration of the research results
Autorzy:
Podhalańska, T.
Waksmundzka, M. I.
Becker, A.
Roszkowska-Remin, J.
Dyrka, I.
Feldman-Olszewska, A.
Głuszyński, A.
Grotek, I.
Janas, M.
Karcz, P.
Nowak, G.
Pacześna, J.
Roman, M.
Sikorska-Jaworowska, M.
Kuberska, M.
Kozłowska, A.
Sobień, K.
Powiązania:
https://bibliotekanauki.pl/articles/2075500.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
niekonwencjonalne złoża węglowodorów
strefa perspektywiczna
dolny paleozoik
karbon
basen bałtycko-podlasko-lubelski
zagłębie SW Poland
unconventional hydrocarbon resources
prospective zones
lower Palaeozoic
Carboniferous
Baltic-Podlasie-Lublin basin
Carboniferous basin of SW Poland
Opis:
The paper presents the characteristics of prospective zones identified for the first time within the lower Palaeozoic shale formations occurring in the Baltic-Podlasie-Lublin Basin and within the Carboniferous shale, sandstone, and mixed shale-sandstone complexes (the so-called hybrid complexes) in the basin of south-western Poland. The lateral and vertical ranges of these zones are determined based on specific criteria using the results of various research methods and analyses, i.e.: stratigraphic, sedimentological, mineralogical, petrological and geochemical of organic matter, petrographic and petrophysical, including interpretation of well logs. Archived geological materials and those coming from the boreholes drilled recently in the concession areas were also used. Four prospective zones have been distinguished in the lower Palaeozoic of the so-called shale belt: SP1, SP2, SP3 and SP4. The most prospective area for the occurrence of unconventional hydrocarbon deposits in shale formations is the Baltic region – the Łeba Elevation, where there are all four perspective zones, only partially covering the range of potentially prospective formations. In each of these zones, both liquid and gas hydrocarbons can be expected in this area. Due to the low percentage of organic matter, the lowest hydrocarbon generation potential is attributed to the Lublin region. However, the low values of this parameter are compensated by other parameters, i.e. the considerable thickness and lateral extent of zone SP4 corresponding partly to the Pelplin Formation. In the Carboniferous rocks of south-western Poland, seven prospective zones have been distinguished in four borehole sections. Four of them are “tight” zones in compact sandstones, while the other three zones represent a hybrid type in complexes with mixed lithology. No prospective zones have been defined in complexes with homogeneous shale lithologies. Determination of lateral extents of the identified zones has not been possible due to the scarcity of data on the geological structure and stratigraphy of the Carboniferous succession in the study area
Źródło:
Przegląd Geologiczny; 2016, 64, 12; 1008--1021
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zasoby przewidywane surowców metalicznych Polski na mapie w skali 1 : 200 000 – miedź, srebro, złoto, platyna i pallad w utworach cechsztyńskiej serii miedzionośnej
Predicted metallic resources in Poland presented on the prospective maps at scale 1 : 200 000 – copper, silver, gold, platinum and palladium in the Kupferschiefer ore series
Autorzy:
Oszczepalski, S.
Chmielewski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075350.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Cu-Ag
Au-Pt-Pd
obszary perspektywiczne
przewidywane środki
seria miedzionośna
SW Polska
prospective areas
predicted resources
Kupferschiefer
SW Poland
Opis:
Themost significant copper reserves in Poland are confined to sediment-hosted stratiform Kupferschiefer-type deposits that occur at the Zechstein/Rotliegend transition. Gradual depletion of shallow reserves in the Fore-Sudetic Monocline results in exploration of deeper beds, and the long-term challenges require new solutions for mining industry of the future and industrial market within the EU, to enable the reindustrialization of Europe. Latest studies of numerous drillhole cores strongly indicate that the Kupferschiefer series in SW Poland (outside the Lubin–Sieroszowice Copper District) contains a very large volume of prognostic, prospective and hypothetical resources. Thirty Cu-Ag prospects have been delineated (including six areas with prognostic resources, six with prospective resources, and 18 areas with hypothetical resources). Among the prospective areas, particular attention is paid to the areas with prognostic resources (Bia³o³êka, Grochowice, Krêpa, Kulów, Luboszyce), adjacent to the existing mines of the Lubin–Sieroszowice copper district. The areas of Nowiny, Mirków, Raciborowice and ¯arków are also interesting due to accessible depths, and the Bogdaj, Henrykowice, Janowo and Sulmierzyce areas due to considerable resources and reasonable depth. Extremely interesting is the possibility of extension of the Bytom Odrzañski deposit towards the Jany, Mozów and Wilcze prospective areas. Studies of archival drillhole cores taken outside the documented Cu-Ag Lubin–Sieroszowice deposit revealed Rote-Fäule-related Au-Pt-Pd mineralization in many localities of SW Poland. Fifteen Au prospective areas, accompanied by Pt-Pd mineralization, have been delineated. However, due to relatively low thickness and content, Au-Pt-Pd mineralization can be considered only as associated with the overlying Cu-Ag ores. It can be estimated that approximately 166 million Mg Cu and 269 thousand Mg Ag concentrated as predicted resources in prospects of SW Poland for future mining, which will be possible, when geological and technological barriers (depth, temperature, oil and gas) will meet economic trends in the world market.
Źródło:
Przegląd Geologiczny; 2015, 63, 9; 534--545
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowe dane o wieku i petrologii kenozoicznych bazaltoidów dolnośląskich
New data on age and petrological properties of Lower Silesian Cenozoic basaltoids, SW Poland
Autorzy:
Badura, J.
Pécskay, Z.
Koszowska, E.
Wolska, A.
Zuchiewicz, W.
Przybylski, B.
Powiązania:
https://bibliotekanauki.pl/articles/2074475.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
bazaltoidy
petrologia
geochemia
kenozoik
Dolny Śląsk
basaltoids
K-Ar dating
petrology
geochemistry
Cenozoic
Lower Silesia
SW Poland
Opis:
Fifteen samples of basaltoid rocks have been analysed from the Lower Silesia, SW Poland, some of them from localities close to the Sudetic Marginal Fault. K-Ar datings have been made on whole rock samples, using the methodology applied by the Institute of Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary. Most of the samples give ages ranging between 21- 38 Ma, whereas that derived from a borehole in the Mokrzeszów Graben has been dated to 44 Ma. Another borehole sample (Jeżów Sudecki B-5), close to the Intrasudetic Fault, is of 59 Ma age. On the other hand, the supposedly "Quaternary" basaltoids from Dębowiec area fall into the interval of 29–30 Ma. The southeasternmost occurrences of the Lower Silesian basaltoids at Nowa Cerekiew display two generations of effusive activity: the older lava flows (26 Ma) are cut by plugs dated to 22 Ma. The Oligocene–Lower Miocene (26-33 Ma, 20'24 Ma) rocks represent alkali basalts and basanites. The alkali basalts consist of phenocrysts of olivine (chrysolite), altered to a different degree, and clinopyroxene (salite). In the matrix, clinopyroxene (Ti-salite), olivine (hyalosiderite), plagioclases (labradorite–andesine), and opaque minerals (titanomagnetite, ilmenite) occur. The basanites contain phenocrysts of altered olivine (chrysolite) and clinopyroxene (salite). Their matrix consists of clinopyroxene (Ti-salites), olivine (hyalosiderite), nepheline, plagioclases (bytownite–andesine), and opaque minerals. On the TAS diagram, samples of the studied basaltoids plot mainly in the fields of basalts and basanites/tephrites. The bimodality of some samples falling into two fields of basalts and basanites/nephelinites on the TiO2/Zr-Nb/y diagram results from their distinct geochemical signature.
Źródło:
Przegląd Geologiczny; 2006, 54, 2; 145-153
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrografia i mineralogia łupków niższego paleozoiku kratonu wschodnioeuropejskiego oraz piaskowców karbonu podłoża monokliny przedsudeckiej
Petrography and mineralogy of the lower Palaeozoic shales from the East European Craton and Carboniferous sandstones from the basement of the Fore-Sudetic Homocline
Autorzy:
Sikorska-Jaworowska, M.
Kuberska, M.
Kozłowska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075495.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
petrologia
dolny paleozoik
Karbon
kraton wschodnioeuropejski
SW Polska
niekonwencjonalne węglowodory
petrology
lower Palaeozoic
Carboniferous
East European Craton
SW Poland
unconventional hydrocarbons
Opis:
The study deals with clay-silt shales occurring in the lower Palaeozoic basin at the western slope of the East European Craton, and sandstones known from the Carboniferous Basin of SW Poland (basement of theFore-SudeticHomocline).The clay groundmass of the shales consistslargely of illite, and the silt fraction is made up of quartz with a variable admixture of feldspars. Quartz and carbonate cements are common, while pyrite, kaolinite and phosphate cements are rare. The clay groundmass reveals microporosity in the form of microchannels paralleling illite plates, and visible with in mica packets. Carboniferous sandstones are represented mostly by sublithic or subarkosic wackes and rarely by lithic, sublithic or subarkosic arenites. The pore space between sand grains is completely filled by clayey matrix. Both porosity and permeability are very low in the sandstones.
Źródło:
Przegląd Geologiczny; 2016, 64, 12; 963--967
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Osuwiska w Sudetach
Landslides in the Sudetes
Autorzy:
Sikora, Rafał
Wojciechowski, Tomasz
Powiązania:
https://bibliotekanauki.pl/articles/2075936.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ruchy masowe
cyfrowy model wysokościowy
mapa podatności na osuwiska
SW Poland
mass movements
digital elevation model
landslide susceptibility map
Opis:
This paper presents the results of analysis of landslides distribution in the Sudetes (SW Poland). Our study was based on the analysis of the LiDAR-data digital elevation model and integrated with investigations of different factors for landslide development. The results of the study showed relationships between the spatial distribution of landslides and geology of their basement. For the areas built by Permo-Mesozoic and late Variscan sedimentary and volcanogenic rocks, the tectonic and lithological factors are predominant for landslide occurrences. The largest landslides have a tectonic affinity and represent a frontal type of geometry. The relationships between geological conditions and mass movements were also confirmed by the constructed landslide susceptibility map of the Sudetes.
Źródło:
Przegląd Geologiczny; 2019, 67, 5; 360--368
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Przydatność pomiarów georadarowych i analiz geomorfometrycznych do rozpoznania wewnętrznej struktury płytkich osuwisk : na przykładzie góry Średniak w Masywie Śnieżnika, Sudety Wschodnie
Evaluation of usefulness of integrated ground-penetrating radar and geomorphometric analyses applied to recognition of internal structure of shallow landslides - case study from
Autorzy:
Makoś, M.
Sobczyk, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075801.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
georadar
analiza geomorfometryczna
translacyjne osuwisko
wewnętrzna architektura osuwisk
Sudety Wschodnie
SW Polska
ground-penetratingradar
geomorphometric analysis
translational landslide
internal architecture of landslide deposits
Eastern Sudetes
SW Poland
Opis:
The paper reviews an application of non-destructive electromagnetic imaging of shallow bedrock and landslide colluvium horizons performed with ground-penetrating radar (GPR) technique on mass movement-affected mountain slope. We used a non-shielded 52 MHz GPR equipment to study an area of a shallow translational landslide, which developed on steeply inclined gneissic bedrock on Mt. Sredniak slopes (1210 m a.s.l.) in the Śnieżnik Massif. This landslide originated at the boundary zone between intact bedrock comprising Proterozoic gneisses and uppermost slope cover, as a result of continuous rainfall during July of 2011. Furthermore, to better understand and examine a landslide area on Mt. Sredniak slopes we also applied structural geological and geomorphological methods. The GPR analyses resulted in high-resolution imaging of internal slope structure and gravitational deposit architecture in the range of 0.5-5 m below surface level. Electromagnetic sounding performed directly above the landslide source area elucidated a set of bedrock discontinuities with a possible direct impact on water aggregation and migration during the rainfall episodes. Furthermore, a GPR profile performed in a landslide toe area, showed subsurface reflection horizons to be correlated with a colluvium/bedrock transitional zone and internal heterogeneous architecture of colluvial deposits. Ground-penetrating radar proved to be both powerful and an easy-maintained 'on-site' method for steep mountain slope analysis, with a potential for high-resolution imaging of shallow-seated gravitational slope deformations.
Źródło:
Przegląd Geologiczny; 2018, 66, 10; 636--647
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Local and exotic building and decorative stones in historical castles of SW Poland : a reconnaissance study
Autorzy:
Kryza, R.
Dziedzic, M.
Unterwurzacher, M.
Prell, M.
Pietrzykowska, K.
Strick, D.
Schumacher, V.
Wilhelm, D.
Powiązania:
https://bibliotekanauki.pl/articles/2066809.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
castles
Lower Silesia
SW Poland
building stone
decorative stone
architectural heritage
cultural heritage
zamek
Dolny Śląsk
Polska
kamień budowlany
kamień dekoracyjny
dziedzictwo architektoniczne
dziedzictwo kulturowe
Opis:
South-west Poland (Silesia) is the region of dramatic history which has left significant heritage, comprising, e.g., numerous historical castles. In this paper, we describe selected castles in Lower Silesia, with special attention given to the usage of exotic (imported) decorative stone materials traded across Europe in various historical periods. Out of the total number of c. 100 historical castles and palaces in SW Poland, only three of them, i.e. Czocha, Ksi¹¿ and Moszna, have preserved significant amount of the original stone decoration. In Czocha Castel, apart from local stones, we have identified, e.g.: red and white, and grey limestones (from Belgium, Germany or Italy). In Ksi¹¿ Castle, the interiors have a great variety of exotic stone materials: travertine, marbles and limestones, e.g. Rosso di Francia, and many others, mostly from France and Italy. In Moszna Castle, representative rooms are adorned with “marbles”: Rosso di Verona, Giallo di Verona, Giallo Siena, Rosso di Francia, and serpentinites and ophicalcites (from Austria and Italy). Most of the exotic stones in the three castles studied were imported at the turn of the 19th–20th centuries and in the early 20th century, when the castles were largely reconstructed and redecorated.
Źródło:
Przegląd Geologiczny; 2015, 63, 6; 332--344
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Łupki krystaliczne złóż południowo-zachodniej Polski stosowane jako kamień budowlany : ocena zróżnicowania walorów dekoracyjnych i możliwości ich zastosowania
Slates, phyllites and schists from deposits of SW Poland used as dimension stones : evaluation of their decorativeness and the possibilities of use
Autorzy:
Stańczak, G.
Powiązania:
https://bibliotekanauki.pl/articles/2075462.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
łupek
fyllit
łupki miki
łupek kwarcytowy
dekoracyjność
tłuczeń
łom
elewacje z kamienia
Dolny Śląsk
Polska
slates
phyllites
mica schists
quartzitic schists
decorativeness
broken stone
ashlar
stone cladding
Lower Silesian Block
SW Poland
Opis:
In modern architecture, slates, phyllites and schists are becoming more and more popular, and the example of Polish deposits of slates, phyllites and schists indicates that, in the last 10 years, the traditional method of using these rocks as raw material, e.g. for the production ofgranular surface, silty carriers of plant protection products or refractory material, has become gradually dominated by their use as dimension stones. The paper presents the first ranking of the decorative aspects, carried out for slates, phyllites and schists originating from active deposits: Orlowice, Jawornica, Dewon-Pokrzywna, Jeglowa and Jenków, located in the Sudetic Block and Fore-Sudetic Block (Lower Silesian Block, SW Poland). Evaluation of the decorative aspects of slates, phyllites and schists, which takes into account the colour, textural and structuralfeatures of the rock, its ability to be polished, and petrologic type, revealed that the primary and secondary petrographic types documented in these deposits have a high decorative value, mainly because of attractive colour and structural arrangement of mineral components. It should be noted that in the group of over 150 different varieties of colourful metamorphic slates on the stone market in the European Union, Polish slates, phyllites and schists are characterised by unique colours. Therefore, the high decorative value and unique colours characteristic of the Polish slates, phyllites and schists is their essential trait that conditions their use as decorative stone material with a wide range of applications.
Źródło:
Przegląd Geologiczny; 2016, 64, 10; 833--843
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geologia złóż węgla brunatnego w południowo-zachodniej Wielkopolsce
Geology of lignite deposits in the south-western Wielkopolska region
Autorzy:
Urbański, P.
Widera, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075461.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
węgiel brunatny
złoża węgla brunatnego
Wielkopolska
zachodnia Polska
lignite
lignite deposits
SW Wielkopolska
western Poland
Opis:
The south-western Wielkopolska territory belongs to the richest lignite-bearing areas in Poland. In total, there are estimated over 6.4 billion Mg of lignite possible to extraction. The largest deposits are located in tectonic grabens. Many of currently used lithostrati- graphic units of the Paleogene and Neogene were created in this area. The major lignite seams are of the Middle Miocene age and occur within the Ścinawa Formation - the 2nd Lusatian group, and within the Grey Clays Member (Mid-Polish Member) - the 1st Mid-Polish group. The discussed in detail “Poniec-Krobia” and “Oczkowice’” deposits have very favorable geological and mining as well as chemical and technological parameters. Similarly, large resources, reaching nearly 1 billion Mg of lignite and the average calorific value exceeding 10 MJ/kg, have been determined in the most recent documentation for the “Oczkowice” lignite deposits.
Źródło:
Przegląd Geologiczny; 2016, 64, 10; 791--798
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Czy istnieje mazurska, prawoskrętna strefa podatnego ścinania?
Does the Mazury dextral shear zone exist?
Autorzy:
Cymerman, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2074551.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kompleks mazurski
Litwa
Polska
Mezoprotezoik
struktura
otwory
kinematyka
nasunięcia
ductile thrusting
structures
kinematics
boreholes
Mesoproterozoic
Masuria
NE Poland
SW Lithuania
Opis:
Throughout SW Fennoscandia, numerous approximately W-E trending faults and ductile shear zones have recently been recognized. The regiona--scale zone of strike-slip displacements [Mazury lineament] with a dextral component was referred by many authors as apparently influenced by the distribution of ca. 1.6-1.4 Ga old "anorogenic" intrusions of the Mazury Complex [NE Poland]. However, new detailed structural and kinematics studies of drill-cores from 255 boreholes located throughout NE Poland and SW Lithuania [Lazdijai region] indicate that the Mazury Complex, the Suwałki Anorthosite Massif and surrounding lithotectonic domains share a common ductile thrusting deformation, calling into question the concept of a large-scale dextral shear zone and also the "anorogenic" origin hypothesis of the Mazury Complex. One important advance has been the accumulation of structural and kinematics information that allows assessment of the main orogenic transport direction commonly towards the SW, locally to the NE [e.g., in the eastern part of the Suwałki Anorthosite Massif]. This assessment has been coupled with the recognition of the role of major and numerous ductile shear zones within the western part of the East European Platform. In general, compressional deformation with ductile thrusting predominated in the western part of the East European Platform. Very probable strike of regional mylonitic foliation [S1] from almost 100 boreholes has been established, based on geophysical measurements of the curvature of borehole axis and a few tens oriented core samples [SW Lithuania]. It is assumed that the crystalline rocks of NE Poland and SW Lithuania [Lazdijai region] were subjected to similar ductile thrusting to transpressional deformation during the late Gothian [or newly defined Dano-Polonian] orogeny [ca. 1.5 Ga].
Źródło:
Przegląd Geologiczny; 2007, 55, 2; 157-167
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geopark Krajowy – kluczem do sukcesu geoturystyki
National Geopark is key to a successful geotourism
Autorzy:
Kondej, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074858.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geoparki
geostanowiska
Polski Geopark Krajowy
Geopark Łuk Mużakowa
Geopark Góry Św. Anny
Karkonoski Krajowy Geopark
geoparks
geosites
Poland National Geopark
Muskau Arch Geopark
St. Anne's Mountain Geopark
Karkonosze National Geopark
Opis:
Geoparks include objects of inanimate nature, which deserve conservation due to their unique scientific, educational, historical and tourist values. The network supports an idea of the sustainable development and there should be created and promoted by local societies and authorities. The creation of geoparks is a chance on the geoturistic development. In Poland, the initiative to create Nationals Geoparks was developed in 2009 by Henryk Jacek Jezierski The Chief State Geologist, Under Secretary of State in the Ministry of the Environment. A necessary condition of the success of the project is to popularize the knowledge about geology of the region. It seems that a key factor is the ability to the cooperation of authorities, the local community and the private business. Since 2009 the Ministry of the Environment has issued 3 certificates. The prestige position is possessed by the Muskau Arch Geopark established in 2009. In 2010 resultant two following St. Anne's Mountain Geopark and Karkonosze National Geopark were created
Źródło:
Przegląd Geologiczny; 2011, 59, 4; 271-275
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
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