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    Wyświetlanie 1-8 z 8
    Tytuł:
    Kartowanie i modelowanie wgłębne do celów poszukiwań naftowych, podziemnego składowania dwutlenku węgla i geotermii w Polsce : rezultaty, narzędzia i potencjał
    Subsurface mapping and modelling for petroleum prospecting, CCS and geothermics in Poland : results, tools and potential
    Autorzy:
    Papiernik, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075112.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    modele statyczne
    cyfrowe odwzorowanie
    siatka 2D
    siatka 3D
    static models
    digital mapping
    2D grid
    3D grid
    Opis:
    Digital subsurface mapping on a wide scale started in Poland at the beginning of the 1990s. A team of the Department of Fossil Fuels was engaged in this activity from its beginning. In the first stage simple techniques were based on digitalization of archival maps, which gradually were replaced by development of local and regional maps based on 2D grids. In that period the most significant achievements of the team were Geothermal Atlases of the Polish Lowlands. After 2006, 3D grid-based techniques, comprising static structural and parametric models, gradually replaced the 2D grid-based techniques. They were used in completion of the 3D grid-based models lying behind the maps presented in Geothermal Atlases of the western part of the Polish Carpathians, the Carpathian Foredeep and the eastern part of the Polish Carpathians. According to the world trends in the field of petroleum geology, quantitative petroleum resources assessments were carried out using 2D, 2.5 and 3D grid-based generation, migration and expulsion models. At the same time, numerous 3D static models for CCS purposed were developed. At present, our research moves toward better data integration, uncertainty assessment and 4D modelling for petroleum geology (especially unconventional hydrocarbons), geothermal resources and CCS purposes.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 12; 856--861
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rola modelowania strukturalno-parametrycznego w procesie typowania potencjalnej lokalizacji zamkniętych systemów geotermicznych w skałach osadowych
    The role of structural and parametricmodelling in the process of selecting Enhanced Geothermal System location in sedimentary rocks
    Autorzy:
    Sowiżdżał, A.
    Papiernik, B.
    Machowski, G.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075150.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    geothermal energy
    hot dry rocks
    EGS systems
    Enhanced Geothermal System
    sedimentary rocks
    3D modelling
    energia geotermalna
    sucha skała
    gorąca skała
    zamknięty system geotermiczny
    systemy EGS
    skały osadowe
    modelowanie 3D
    Opis:
    In the years 2010–2013, analysis of rocks that build the sedimentary covers in Poland was carried out from the point of view of utilization of energy accumulated in closed geothermal systems – so-called Enhanced Geothermal Systems (EGS). Preliminary assessment of available digital cartographic data in terms of variability in the structural setting, thickness, and geothermal and reservoir parameters allowed selecting, for detailed studies, an area situated in central Poland in the Kujawy segment of the Mid-Polish Anticlinorium, in the Mogilno-£ódŸ Trough and in the northern margin of the Fore-Sudetic Monocline. A complex structural- parametric model was constructed for this area, which comprised the interval from the base of the Carboniferous up to the base of the Cenozoic. The model was a basis for further modelling (e.g. others, modelling of the electric and thermal energy production potential). The study results indicate that the most favourable conditions for the development of EGS occur in the Lower and Middle Buntsandstein deposits to the NE of the K³odawa salt diapir (in the Krooeniewice–Kutno vicinity). They are buried to depths greater than 5000 m b.s.l., their thicknesses exceed 1000 m and they are characterised by porosity about 2.5%, permeability about 0.1 mD and mean density approximately 2.7 g/cm3.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 6; 303--307
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Computer-aided quantitative subsurface mapping : examples of utilization
    Autorzy:
    Papiernik, B.
    Hajto, M.
    Górecki, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/2065891.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    subsurface mapping
    grid
    quantitative map
    Z-MAP Plus
    Opis:
    The present age of digital subsurface mapping is represented above all by quantitative maps based on regular grids. They are created on the basis of various input data: digitized contours, widely comprehended well data, 2D and 3D seismic, and qualitative geological maps. Scope and the data utilization and the applied methodology of processing are strictly dependent on the scale and purpose of a given map; for regional and detailed maps they are significantly different. However, irrespective of the map scale, correct models, reflecting probable subsurface variability, instead of the input data spatial distribution and applied estimation algorithm themselves, are conditioned by chances of integrating of all the mentioned types of data. These purposes can be achieved only through the application of the most flexible interpretive programs such as ZMAP–Plus or mapping modules of the Geographix system. High quality quantitative subsurface maps based on regular grids are nowadays used first of all in petroleum exploration and geothermal research. But development of such studies may contribute to creation of high-quality, interactive, subsurface models, available not only for owners of expensive professional software but also for all geoscientists interested in these topics.
    Źródło:
    Przegląd Geologiczny; 2005, 53, 10/2; 956-960
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Koncepcja rozwoju cyfrowego modelowania budowy geologicznej Polski
    Autorzy:
    Jarosiński, M.
    Papiernik, B.
    Szynkaruk, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2066623.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    modelowanie procesów geologicznych
    struktura geologiczna
    procesy geologiczne
    modeling geological processes
    geological structure
    geological processes
    Opis:
    [...]prezentacja zaawansowania i metod konstrukcji oraz ocena efektywnooeci (stopieñ wykorzystania i koszty) wytworzenia cyfrowych modeli budowy geologicznej. Przyczyniło się to do głębszego, praktycznego wglądu w tę dziedzinę działań europejskich służb geologicznych na etapie, kiedy w Polsce jesteśmy jeszcze przed zasadniczymi decyzjami dotyczącymi inwestycji w rozwój takich modeli w skali kraju. Po dwóch latach od tego spotkania zainicjowane zostały istotne działania w celu realizacji programu cyfryzacji budowy geologicznej Polski. Rozwój cyfrowej kartografii wgłębnej, sformułowany w strategii Głębokich Badań Geologicznych na lata 2008–2015, ogłoszonej przez Ministerstwo Środowiska (Jarosiński & Warias, 2008) przewiduje, że „Poziom rozwoju technologii komputerowej oraz rynek odbiorców, uzasadnia konieczność rozwinięcia tych działań modeli cyfrowych] na dużą skalę.[...]
    Źródło:
    Przegląd Geologiczny; 2014, 62, 12; 801--805
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Wstępne wyniki modelowań przestrzennych (3D) parametrów petrofizycznych skał podczas poszukiwań stref występowania gazu zamkniętego w polskim basenie czerwonego spągowca
    Preliminary results of 3D modeling of petrophysical parameters for tight gas prospecting in the Polish Rotliegend Basin
    Autorzy:
    Papiernik, B.
    Górecki, W.
    Pasternacki, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074766.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    model 3D
    modelowanie facji
    model petrofizyczny
    gaz zamknięty
    czerwony spągowiec
    3D model
    facies modeling
    petrophysical modeling
    tight gas
    Rotliegend
    Opis:
    The Rotliegend Basin is filled with terrigenic complex over 1200 m in thickness. The complex comprises sediments of eolian, fluvial and playa depositional systems (Fig. 1). Reservoir volume of the pore space accessible for the reservoir media is ca. 830-990 km3. Gas exploration in this stratigraphic unit is now focused at depths of around 3000-3800 m b.s.l., in the near-top zone. Poor reservoir properties, especially permeabilities, are here the limiting factor for conventional exploration. A change in the prospecting strategy to comprise tight gas targets moves research into the deeper zone covering the whole profile of the Rotliegend. The paper presents preliminary results of 3D modeling of lithofacies and related petrophysical parameters variability. The static model was created with the use of Petrel 2009.2. Structural framework was built using regional structural, isopach and facies maps. It was relatively detailed, comprising 9 576 000 cells organized in 3 zones and 60 layers. To estimate facies model, the authors used results of integrated environmental analysis of core data and logs from 117 wells (Fig. 2 ). Models of clay content (Vsh) and porosity (PHI) were based on logs from 75 wells. The obtained results show that the northern margin of the Eastern Erg is characterized by presence of numerous eolian strata with porosity ranging from 5 to 15%. Their quality, quantity and thickness decrease toward the north, along with increase in depth. Modeling results indicate that the dominating porous layers of eolian sandstones and fluvial inserts are often intercalated with "non-reservoir" layers revealing porosity below 5%. In this zone, a deeper part of the Rotliegend section should be investigated more thoroughly (Fig. 5, 6, 9). The Pomeranian sector of the Central Basin is dominated by playa and fluvial sediments (Fig. 7, 8, 10). Slightly clayey eolian strata make a few, laterally discontinuous intercalations. Gas accumulations could be expected within local, laterally confined interlayers of eolian and fluvial sandstones with porosity of around 5-12%. Due to the location in the near-base part of the Rotliegend section, close to Carboniferous source rocks, they may be filled with gas, forming so-called sweet spots. Probability of gas occurrence in Pomerania is high as indicated by the Międzyzdroje gas field or small accumulation found in Piaski-PIG2 well. The presented preliminary study allowed to test usability of 3D modeling in tight gas prospecting. Fully reliable results will be obtained after increasing precision of the models comprising detailed seismic interpretation, the use of seismic attributes, and inclusion of quantitative data in diagenetic processes and sedimentology of layers in the modeling process.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 4; 352-364
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Budowa geologiczna i geneza mioceńskiego zrębu Ryszkowej Woli w rejonie Sieniawy-Rudki (wschodnia część zapadliska przedkarpackiego) : wyniki interpretacji danych sejsmiki 3D
    Geological structure and origin of the Miocene Ryszkowa Wola Horst (Sieniawa-Rudka area, eastern part of the Carpathian Foredeep Basin) : Results of 3D seismic data interpretation
    Autorzy:
    Krzywiec, P.
    Aleksandrowski, P.
    Ryzner-Siupik, B.
    Papiernik, B.
    Siupik, J.
    Mastalerz, K.
    Wysocka, A.
    Kasiński, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074352.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    zapadlisko przedkarpackie
    miocen
    dane sejsmiczne 3D
    złoża gazu ziemnego
    budowa geologiczna
    Carpathian Foredeep
    Miocene
    strike-slip faults
    3D seismic data
    natural gas reservoirs
    Opis:
    The Miocene Carpathian Foredeep Basin in Poland (CFB) developed in front of the Outer Carpathian fold-and-thrust belt, at the junction of the East European craton and the Palaeozoic platform. Within the upper Badenian through Sarmatian deposits of its eastern part, the CFB hosts numerous gas fields. The gas-bearing Miocene succession is characterised by a shallowing-upward trend of sedimentation and consists of offshore hemipelagic, turbiditic and deltaic and nearshore-to-estuarine facies associa-tions. The foredeep basin formation was largely controlled by the structure of its Neoproterozoic–Early Cambrian basement, especially by NW–SE trending faults inherited from Mesozoic tectonic history of SE Poland (subsidence and inversion of the Mid-Polish Trough). Several NW–SE-elongated, narrow basement pop-up structures developed in the northeasternmost part of the CFB, one of them being the Ryszkowa Wola block. The uplift of the pop-up basement block involved Miocene reactivation of older fault zones and resulted in the formation of a narrow, NW–SE elongated Ryszkowa Wola horst (RWH) above it, within the Miocene strata. A complex system of right-stepping, en-echelon, mainly normal faults of predominantly E–W trend, branching off from the NW–SE-striking boundaries of the RWH, has developed around and above the horst, leading to compartmentalisation of the Miocene succession into numerous, mutually displaced and rotated fault blocks. Such an association of deformation structures recognised from the 3D seismics was interpreted in terms of transpressive conditions with the horizontal maximum tectonic compression axis directed š E–W and a sinistral strike-slip displacements on NW–SE striking faults in the basement. The structural interpretation of the Ryszkowa Wola structure proposed here is in line with published results of analogue modelling of fault patterns in sediments overlying active strike-slip discontinuities in a rigid basement. The basement-cover interaction within the Ryszkowa Wola structure in the area of Sieniawa–Rudka was partly coeval with the Miocene deposition of the CFB infill. The uplift and horizontal displacements of the Ryszkowa Wola basement block modified the local subsidence pattern and the organisation of Miocene depositional systems. The syn-depositional strike-slip fault activity in the basement of the CFB resulted in differential movements and rotations of kinematically linked fault-blocks in the Miocene succession around and above the RWH, leading to the formation of numerous gas traps.
    Źródło:
    Przegląd Geologiczny; 2005, 53, 8; 656--663
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Sukcesja osadowa miocenu w rejonie zrębu Ryszkowej Woli (obszar Sieniawa-Rudka), zapadlisko przedkarpackie: wyniki facjalnej i stratygraficznej interpretacji danych wiertniczych oraz sejsmiki 3D
    Miocene succession at the Ryszkowa Wola high (Sieniawa-Rudka area), Carpathian Foredeep Basin: facies and stratigraphic interpretation of wellbore and 3D seismic data
    Autorzy:
    Mastalerz, K.
    Wysocka, A.
    Krzywiec, P.
    Kasiński, J.
    Aleksandrowski, P.
    Papiernik, B.
    Ryzner-Siupik, B.
    Siupik, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074444.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    miocen
    zapadlisko przedkarpackie
    sedymentacja
    analiza stratygraficzna
    analiza facjalna
    dane wiertnicze
    dane sejsmiczne 3D
    Carpathian Foredeep
    Miocene
    sedimentation
    sequence stratigraphy
    facies analysis
    well log interpretation
    3D seismic data
    Opis:
    The Polish Carpathian Foredeep Basin (PCFB) is the northern compartment of a foreland basin system that surrounds the Carpathian orogenic belt. The axis of the eastern part of the PCFB plunges gently towards SE, where the Miocene basin-fill succession exceeds 2000 metres in thickness. The Miocene succession developed in shallow marine ramp settings and is subdivided into 3 lithostratigraphic units: sub-evaporitic (onshore-to-nearshore), evaporitic, and supra-evaporitic (offshore-to-estuarine). The upper unit includes a siliciclastic series (Upper Badenian–Sarmatian), which constitutes the main segment of the succession. It displays an asymmetric, shallowing-up trend, expressed by the following sequence: hemipelagic-turbiditic-deltaic-low-energy nearshore-to-estuarine facies associations. Sediment accummulation in the basin has been significantly overprinted by higher-frequency cyclicity and encloses several genetic stratigraphic sequences bounded by MFS surfaces. An early phase of the basin development was characterised by high-rate subsidence and slow-rate sedimentation (hemipelagic facies). The turbiditic facies association identified within the Sieniawa–Rudka area resulted from southward progradation of a submarine fan/prodeltaic depositional system, mainly fed from the northern and north–western continental margins of the basin. An overall SE–ward palaeoslope inclination controlled the main phase of the deltaic progradation, which had gradually replaced the turbiditic systems. The late deltaic phase was characterised by ENE palaeotransport directions. The final phase of the basin filling took place in shallow-water, low-energy, nearshore-to-estuarine environments. In the early stage of the basin development, a complex system of NW–SE elongated basement pop-ups and flower structures in the Miocene succession were produced by reactivation and inversion of Mesozoic basement faults. The growth of these positive structures modified local subsidence patterns and affected the organisation of depositional systems of the siliciclastic series. A narrow elevation of the RyszkowaWola High (RWH) gradually grew above one of the pop-up structures. Complex structural-stratigraphic hydrocarbon traps developed along the RWH, due to interaction between the growth of local faults and the development of the successive depositional systems. Tidally-modified delta-top and estuarine facies are the most common hydrocarbon hosts within individual sequences of the „deltaic” segment of the succession..
    Źródło:
    Przegląd Geologiczny; 2006, 54, 4; 333-342
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ewolucja utworów mioceńskich zapadliska przedkarpackiego w rejonie Rzeszowa (obszar zdjęcia sejsmicznego 3D Sokołów-Smolarzyny)
    Evolution of the Miocene deposits of the Carpathian Foredeep in the vicinity of Rzeszów (the Sokołów-Smolarzyny 3D seismic survey area)
    Autorzy:
    Krzywiec, P.
    Wysocka, A.
    Oszczypko, N.
    Mastalerz, K.
    Papiernik, B.
    Wróbel, G.
    Oszczypko-Clowes, M.
    Aleksandrowski, P.
    Madej, K
    Kijewska, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074574.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    zapadlisko przedkarpackie
    miocen
    zdjęcie sejsmiczne 3D
    Carpathian foredeep
    Miocene
    3D seismic data
    Opis:
    The Miocene Carpathian foredeep basin in Poland (CFB) developed in front of the Outer Carpathian fold-and-thrust belt, at the junction of the East European craton and the Palaeozoic platform. 3D seismic data, cores and well logs from Sokołów area (vicinity of Rzeszów) were used in order to construct new depositional model of the Miocene succession of the Carpathian foredeep. The gas-bearing Miocene infill of the CFB is characterized by a shallowing-upward trend of sedimentation and consists of hemipelagic, turbiditic and deltaic and nearshore-to-estuarine facies associations. Lowermost part of the Miocene infill seems to has been deposited from the North. Such direction of sediment supply was related to influence of existing relief of the pre-Miocene basement, where very deep (up to 1,5 km) erosional valleys cut into the pre-Miocene (Precambrian) basement due to inversion and uplift of the SE segment of theMid-Polish Trough are located. Upper part of theMiocene infill reflects sediment progradation from the South, from the Carpathian area into the foredeep basin. In the Rzeszów area existence of the so-called anhydrite-less island, i.e. relatively large area devoid of the Badenian evaporitic cover caused by the post-Badenian uplift and widespread erosion of evaporites,has been postulated for many years. Interpretation of 3D seismic data showed that such model should be abandoned. In the studied part of the CFB, Late Badenian evaporitic sedimentation was restricted to the axial parts of deep paleovalleys. Evaporites deposited in these valleys have been rarely encountered by exploration wells as such wells were almost exclusively located above basement highs separating erosional paleovalleys, hence giving incorrect assumption regarding regional lack of evaporitic cover. It is possible that in axial parts of these valleys important gas accumulations might exist, charged from the South and sealed by the Badenian evaporites.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 3; 232-232
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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