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    Tytuł:
    Sedymentacja utworów miocenu we wschodniej części zapadliska przedkarpackiego
    Miocene deposition in the eastern part of the Carpathian Foredeep in Poland
    Autorzy:
    Dziadzio, P.
    Maksym, A.
    Olszewska, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074465.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    miocen
    stratygrafia
    sedymentacja
    zapadlisko przedkarpackie
    Carpathian Foredeep
    Miocene
    stratigraphy
    depositional sequences
    Opis:
    Results of new biostratigraphical investigations correlated with nannoplankton zones permit to suggest that deposits which are filling the eastern, Polish part of the Carpathian Foredeep Basin include also the late Sarmatian and Panonian deposits. The filling of eastern parts of the Carpathian Foredeep, as in most foredeep basins, took place in two main stages; (1) underfilled flysch stage - lasting from the early Badenian to the lower part of late Badenian (Moravian– Wieliczian) and (2) overfilled molasse stage — lasting from upper part of the late Badenian to Panonian (Kosovian–Meotian). Classically, this flysch to molasse transition is interpreted as a record of the migration of the thrust wedge and foreland basin over the hinge line of the inherited passive margin. Also, the Badenian and Sarmatian successions are characterised by very diverse facies, which were deposited in various depositional environments. A detailed sedimentological analysis of cores, together with well log analysis, and seismic sections permitted to fit the stratigraphic column into a sequence stratigraphic framework. Within this framework, the Badenian and Sarmatian successions are interpreted to have been deposited within 3 third-order depositional sequences: the first two in the Badenian (not recognised in seismic scale), and the third during the Sarmatian, which consists of 4 fourth-order sequences (Dziadzio, 1999, 2000), with total thickness of 800 to over 3000 m. The M3 boundary is interpreted as a flooding surface within the fourth order, oldest Sarmatian depositional sequence. The M2 boundary corresponds to the boundary between two foraminiferal zones Anomalinoides dividens and Varidentella reussi, within the Sarmatian succession, which lies in the upper part of the second Sarmatian sequences, near the maximum flooding surface, in late phase of highstand sea level. The M1 boundary is interpreted as a transgressive surface within the third Sarmatian sequence. The boundary M0 marks transgressive surface within the fourth Sarmatian sequence and also is a stratigraphical boundary between two youngest foraminiferal zones Velapertina reussi and Porosononion granosum, and marks a border between the Wolhynian and Bessarabian stages.
    Źródło:
    Przegląd Geologiczny; 2006, 54, 5; 413-420
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Oil and gas fields in the Carpathians and the Carpathian Foredeep
    Autorzy:
    Górka, A.
    Gliniak, P.
    Madej, K.
    Maksym, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2066022.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    gas fields
    oil fields
    Carpathian Foredeep
    Carpathians
    sub-miocene basement
    reserves
    activity in the South of Poland
    Opis:
    Southeastern Poland is one of the oldest petroleum provinces in the world. Although hydrocarbon production has been conducted in this region since the middle of 19th century, there is still a good potential for more discoveries. 9 billion cubic meters of high methane gas reserves reported in the years 2000-2006, when combined with the previously discovered gas fields, essentially satisfy gas demand for this area. Currently, Miocene deposit of the Carpathian Foredeep is the most prolific exploration target area with more than 100 discoveries of high methane gas. The total reserves of these fields are 138 billion cubic meters, and the cumulative production is more than 90 billion cubic meters of natural gas. Large gas fields in terms of area and reserves that have already been discovered are followed by present discoveries of fields with relatively smaller area, their reserves are up to 2 billion cubic meters. Current exploration efforts are focused on good understanding of the sub-miocene basement configuration as well as detecting of seismic anomalies directly related to natural gas accumulations. Another very important element of exploration strategy for Southern Poland is the Mesozoic and Paleozoic deposits of the Carpathian Foredeep. The most prospective for discovering of sizeable hydrocarbon fields are Cretaceous (Cenomanian) sandstones and Upper Jurassic carbonates, locally also Middle Jurassic sandstone as well as Lower Carboniferous and Devonian carbonates. So far 13 gas fields and 10 oil fields have been discovered in the Mesozoic and Paleozoic of the Carpathian Foredeep and the sub-Carpathian basement with booked reserves of 7.5 billion cubic meters of natural gas and 4.7 million tons of oil. The cumulative production amounts to 6.1 billion cubic meters of gas and 4.3 million tons of oil. Different exploration problems have been encountered in the Carpathians. Most of the fields which have been discovered in the Flysch Carpathians occur in shallow, steep, narrow, commonly thrusted and faulted folds. Oil and gas fields discovered so far in the Carpathians have small reserves. Additionally, discovered and booked reserves of existing oil and gas fields are depleted to a large extent. 17 gas fields and 67 oil fields have been discovered in the Carpathians. Booked reserves amount to 16.6 billion cubic meters of natural gas and 12.3 million tons of oil. Cumulative production has been 15.2 billion cubic meters of gas and 11.9 million tons of oil. To sum up, it should be emphasized that the bulk of gas reserves discovered, booked and developed recently in Southern Poland comes from the autochthonous Miocene deposits. This trend, which involves high methane gas, is expected to continue for the next few years. Potential oil discoveries can be attributed mainly to the flysch Carpathians and Paleozoic, but requires more research and further exploration on a larger scale.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 12/1; 993-998
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-2 z 2

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