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Wyszukujesz frazę "seismic stratigraphy" wg kryterium: Temat


Wyświetlanie 1-5 z 5
Tytuł:
Depositional architecture of the Upper Cretaceous succession in central Poland (Grudziądz-Polik area) based on regional seismic data
Autorzy:
Stachowska, Aleksandra
Krzywiec, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/2059590.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
central Poland
depositional architecture
layer-cake stratigraphy
regional seismic data
seismic stratigraphy
Upper Cretaceous.
Opis:
Interpretation of the regional high-resolution seismic data of the PolandSPANTM survey in the Grudziądz-Polik area revealed a new depositional architecture of the Upper Cretaceous succession that differs substantially from the previously assumed layer-cake model, commonly applied to Permian-Mesozoic sequences. A previously unrecognized regional unconformity, dividing the Upper Cretaceous succession into two units characterized by very different internal geometries, was identified and mapped. The lower unit, with a generally layer-cake internal pattern, is overlain by an upper unit composed of a regionally low-angle succession that pinches out toward the south. This newly revealed regional pattern remained unrecognized in previous regional compilations based on borehole data, which suggested that a layer-cake depositional architecture prevailed throughout the entire Upper Cretaceous. This new image of Upper Cretaceous depositional patterns has far-reaching consequences for understanding of the evolution of the Polish Basin in the Late Cretaceous, including its subsidence and burial history, deposition, and tectonic development. A re-evaluation of the chronostratigraphy of the Upper Cretaceous of the Polish Basin is needed to temporally constrain the succession of sedimentary and tectonic events revealed here.
Źródło:
Geological Quarterly; 2021, 65, 2; 65: 21
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Seismic stratigraphic analysis for hydrocarbon exploration in the Beta Field, Coastal Swamp Depobelt, Niger Delta
Autorzy:
Adeleye, Mutiu A.
Yekeen, Kazeem O.
Amidu, Sikiru A.
Powiązania:
https://bibliotekanauki.pl/articles/1841773.pdf
Data publikacji:
2020
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
seismic stratigraphy
system tracts
sequence boundary
depositional sequences
reservoir presence
Nigeria
Opis:
Hydrocarbon exploration analysis from a seismic stratigraphic approach was carried out within the Beta Field, Coastal Swamp Depobelt, Niger Delta, to identify system tracts and sequence boundaries that could be associated with potential hydrocarbon accumulation. 3D seismic volume and data from four wells were analyzed. Depositional sequences, system tracts, sequence boundaries, and candidate maximum flooding surfaces were picked from logs, while reflection patterns and terminations were interpreted from seismic sections. Log shapes from gamma rays in combination with seismic facies analysis were interpreted in order to delineate lithology, depositional environments and depositional sequences. Seismic attributes were extracted and were draped on gridded surfaces from the interpreted seismic horizons. These were integrated with structure maps to obtain structural and stratigraphic trends, and possible presence of reservoir sand. Five depositional sequences and nine seismic facies were identified within the field. The depositional sequences were designated Sequences S1 to S5 based on the depth of the occurrences and stacking patterns. This study reveals a progression from fluvial depositional settings to the shelf. The main reservoirs identified are the sand units of the highstand and lowstand within three depositional sequences (S1, S4 and S5) although interbedded sands within the TST of S4 and S5 are also suspected of being potential reservoirs. The channel sand deposits within the study area are suspected to be hydrocarbon bearing as they occurred within the complex fault trapping system popular in the Niger Delta. The application of seismic stratigraphy, as shown in this study, serves to encourage exploration in the Niger Delta where it could be effectively employed for reducing risk in hydrocarbon exploration.
Źródło:
Geology, Geophysics and Environment; 2020, 46, 4; 259-271
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structural and seismic sequence stratigraphy analysis of seismic and biostratigraphy data from an onshore field, Niger Delta, Nigeria
Autorzy:
Emujakporue, G. O.
Eyo, A. J.
Powiązania:
https://bibliotekanauki.pl/articles/1078525.pdf
Data publikacji:
2019
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Niger Delta
Sequence stratigraphy
faults
horzons
seismic
Opis:
The structural and sequence stratigraphy of a Niger Delta onshore field has been analysed from seismic and biostratigraphy data in order to assess the hydrocarbon potential of the area. Seven faults F1, F2, F3, F4, F5, F6 and F7 were delineated in the seismic sections. The faults, F1, F4, F6 and F7 are synthetic faults, while F2, F3 and F5 are antithetic. Two horizons H1 and H2 were identified in the seismic sections within the time window of 2200-2600 ms. The seismic sequence stratigraphy analysis revealed five sequence boundaries S1, S2, S3, S4 and S5, which represent four depositional sequences. Four maximum flooding surfaces (MFS) were also delineated in the seismic data. The analysis of the biostratigraphy data thus revealed four sequence boundaries (S1, S2, S3, S4) and three maximum surfaces (MFS1, MFS2 and MF3). The age of the sequence boundary ranges from 13.1Ma to 8.3 Ma. The age of the observed maximum flooding surfaces ranges from 12.8 Ma to 9.4 Ma. In vertical succession, the depositional sequences were identified by the order; sequence boundary, lowstand system tract (LST), Transgressive system tract (TST), Maximum flooding surface (MFS), and Highstand system tract (HST). The lowstand system tract is made up of stacking pattern of sand, while the transgressive system tract thinned into the condense section.
Źródło:
World News of Natural Sciences; 2019, 22; 190-199
2543-5426
Pojawia się w:
World News of Natural Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sposób korelacji anomalii sejsmicznych z informacją otworową w analizie sedymentologicznej rejonu Pustków–Sędziszów (południowa część zapadliska przedkarpackiego)
Method of seismic anomalies correlation with the well information for sedimentology analysis of Pustków–Sędziszów area (southern part of the Carpathian Foredeep)
Autorzy:
Stankiewicz, B.
Dzwinel, K.
Pasek, P.
Powiązania:
https://bibliotekanauki.pl/articles/2063146.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
sejsmika 3D
anomalia sejsmiczna
geofizyka otworowa
stratygrafia sekwencji
miocen
zapadlisko przedkarpackie
3D seismic data
seismic anomaly
well log
sequence stratigraphy
Miocene
Carpathian Foredeep
Opis:
Zintegrowana analiza anomalii sejsmicznych wraz z interpretacją danych geofizyki otworowej dała podstawy do odtworzenia środowiska sedymentacji osadów mioceńskich zapadliska przedkarpackiego. Zmienność wykształcenia osadów, zarówno pionową, jak i poziomą, prześledzono na podstawie szczegółowej korelacji międzyotworowej, a następnie, wykorzystując dodatkowo analizę charakteru wykształcenia krzywych geofizyki otworowej, dokonano próby określenia zarysu architektury depozycyjnej. W celu odtworzenia środowiska sedymentacji na większym obszarze, posłużono się szczegółową interpretacją zdjęcia sejsmicznego 3D. Analiza form geoanomalii i badanie spójności zapisu sejsmicznego zaowocowało wydzieleniem różnych elementów paleomorfologii, takich jak: koryta, wały przybrzeżne, stożki i litosomy.
Integrated analysis of seismic anomalies together with well logging data interpretation was a basis for reconstruction of processes of depositional environment of the Miocene succession, in the Carpathian Foredeep. Vertical and lateral variability of sediments was analysed using detailed wells correlation. Then, using the analysis of a shape of well logs, the outline of depositional architecture was determined. In order to determine the sedimentology environment in a larger area, the detailed 3D seismic data results interpretation was used. The analysis of geoanomalies forms and coherence of seismic record resulted in differentiation of various paleomorphology elements such as: channels, subaqueous levees, fans and lithosom.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2010, 439 (2); 417--421
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
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
    Wyświetlanie 1-5 z 5

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