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Wyświetlanie 1-10 z 10
Tytuł:
Exploration and exploitation of oil and gas fields in Poland: a historical outline
Autorzy:
Karnkowski, P.
Powiązania:
https://bibliotekanauki.pl/articles/2066017.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
historia przemysłu naftowego
pola naftowe i gazowe
Karpaty
zapadlisko przedkarpackie
nizina polska
history of petroleum industry
oil and gas fields in Poland
Carpathians
Carpathian Foredeep
Polish Lowland
Opis:
Petroleum industry began in Galicia region, the former part of Poland which was in 1772-1918 a province of the Austro-Hungarian Empire. The birth of this industry was connected with petroleum distillation made by two pharmacists: Ignacy Łukasiewicz and Jan Zeh, who persistently were working to get a liquid without both light and heavy factions of hydrocarbons, i.e. a liquid paraffin of oil. This aim was reached in spring of 1853. That time also a kerosene lamp was constructed by Adam Bratkowski under direction of I. Łukasiewicz. The set of these lamps was used in the Lviv municipal hospital during the serious surgical operation on 31 July 1853. This date was accepted as the beginning of the world oil industry. Next year I. Lukasiewicz established the oil mine in the Bóbrka village near Krosno. Oil wells then were frequently the open ones dug out to the depth of 60 m and from them oil was extracted with wooden buckets by usage of gin. When petroleum deliveries were assured I. Łukasiewicz founded in 1856 the first petroleum distillery in Ulaszowice near Jasło, the second one in 1858 in Kleczany, and the third one in Polanka near Krosno in 1861. In 1890s in the Carpathians the new oil deposits were discovered in the Gorlice-Jasło-Sanok region. In 1888 the Bergheim Mac Garvey Company found the new oil fields in Weglówka near Krosno and the Galician Oil Mining Company discovered oil-rich deposits in Potok, Turaszówka, Iwonicz, Stara Wieś, Rudawka Rymanowska and Wankowa. Discoveries were also along the Carpathians thrust front where exists the zone of deep-seated folds covered by the Miocene deposits. Oil fields are here located at depth of 800-2000 m. In the Borislav vicinity a few very efficient oil fields were documented in 1896. In 1908 the highly productive "Oil City" well with oil production 2500 t/d was drilled. Exploitation in this region of the Carpathians in 1909 was 2x10exp.6 t, i.e. 5%of the world oil production and Galicia was the third producer in the world. During 150 years of exploration, in this part of Polish Carpathians, 67 oil and 17 gas fields were discovered. In the Carpathian Foredeep 50 gas fields and 10 oil fields were documented. The biggest success was the Jaksmanice-Przemyśl gas field with 75x 10exp.9 m3 of resources. In the Polish Lowland in 1946, just after the Second World War, basing on gravimetric and magnetic data, the first drilling was located on the Kłodawa structure and the Zechstein salts at depth of 300 m were found. Later this drill was a base for foundation of Kłodawa salt mine. In 1961 in the Fore-Sudetic Monocline the first oil field Rybaki was discovered in the Zechstein Main Dolomite formation, and three years later, in 1964, the first gas field discovery - Bogdaj-Uciechów was found within the Rotliegend sandstone and the Zechstein Limestone unit. Until now a dozen of oil and gas fields were documented not only in the Permian formations but also in the Devonian and the Carboniferous deposits in the Lublin Petroleum Province and in the Cambrian sandstones in the Gdansk Petroleum Province. Exploration works, initiated after the Second World War, both in the Carpathians as well as in the Carpathian Foreland and the Polish Lowland give premises of new oil and gas filed discoveries there also in the future.
Źródło:
Przegląd Geologiczny; 2007, 55, 12/1; 1049-1059
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geneza i ewolucja polskiego basenu czerwonego spągowca
Autorzy:
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/1204877.pdf
Data publikacji:
1999
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
polski basen
czerwony spągowiec
analiza basenów sedymentacyjnych
stratygrafia
paleogeografia
system naftowy
Polish Basin
Rotliegend
basin analysis
stratigraphy
palaeogeography
petroleum play
Opis:
Polski basen czerwonego spągowca (PBCS) jest częścią wielkiego basenu sedymentacyjnego zwanego południowym basenem permskim, leżącym w zachodniej i centralnej Europie. Historia rozwoju polskiego basenu czerwonego spągowca rozpoczęła się na przełomie karbonu i permu. Jednak w jego rozwoju można odnaleźć pewne elementy zakorzenione w już przedpermskim paleozoiku. Rozwój sedymentacji w polskim basenie czerwonego spągowca był kontrolowany głównie przez tektonikę i klimat. Wyraźna zmiana klimatyczna, z warunków wilgotnych na suche, nastąpiła dopiero w górnym czerwonym spągowcu (i to nie w jego najniższej części). Ruchy tektoniczne zaznaczały się natomiast poprzez tworzenie miąższych kompleksów zlepieńców. Takie spojrzenie na opracowywaną sukcesję osadów czerwonego spągowca umożliwiło wyróżnienie kilku sekwencji. Ewolucja polskiego basenu czerwonego spągowca nie skończyła się wraz z transgresją cechsztyńską. Wypełnienie PBCS podlegało dalszej ewolucji związanej z rozwojem polskiego basenu permsko-mezozoicznego. Aby móc śledzić ewolucję wypełnienia PBCS wykonano dla tego obszaru analizę historii pogrążania i analizę historii termicznej. Historia subsydencji basenu polskiego na omawianym obszarze pokazuje, że okres późnego permu i triasu były główna fazę ryftowania, a późniejszy rozwój basenu wynika głównie z relaksacji termicznej. Analizując historię termiczną basenu polskiego widać, że w czerwonym spągowcu występowały tam wielkie anomalie geotermiczne. Anomalie te charakteryzowały się wysoką wartością strumienia cieplnego (100-150 mWm-2) w czasie późnego permu i triasu. Tak wysokie wartości odpowiadają przeważnie synryftowemu etapowi rozwoju basenu. W czasie późnego triasu i jury wystąpiło pewne schłodzenie pola cieplnego, ale punktem zwrotnym w historii termicznej basenu polskiego było pogranicze jury i kredy, kiedy południowo-zachodnia część omawianego basenu została znacznie wyniesiona i zerodowana. Wtedy to wartość powierzchniowego strumienia cieplnego w południowo-zachodniej Polsce istotnie zmalała, a wyraźne cechy termiczne poprzedniej epoki zostały zatarte. Występowanie złóż gazu w osadach czerwonego spągowca ograniczone jest do najwyższej części sekwencji osadowej. Skład gazu ziemnego wykazuje niekiedy znaczne zaazotowanie oraz istotne wzbogacenie w hel. Najwyższe koncentracje helu w gazie ziemnym, tak pod względem objętościowym jak i ilościowym, są zlokalizowane w tym samym miejscu, co permsko-jurajska wysoka anomalia geotermiczna i jednocześnie tutaj najpłycej występuje powierzchnia Moho w Polsce. Wyniki analizy historii pogrążenia i historii termicznej analizowanej części basenu polskiego, jak również konfiguracja powierzchni Moho i związane z nią anomalie paleogeotermiczne oraz wysokie koncentracje helu wskazują na asymetryczny model budowy basenu. Strefa wysokich anomalii paleogeotermicznych, rozciągająca się od obszaru między Wrocławiem i Poznaniem i dalej na zachód, była zapewne głównym obszarem ryftowania. Pierwszym etapem rozwoju polskiego basenu ryftowego był wulkanizm, a następnie sedymentacja w czasie czerwonego spągowca.
Źródło:
Polish Geological Institute Special Papers; 1999, 3; 1-93
1507-9791
Pojawia się w:
Polish Geological Institute Special Papers
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petroleum Provinces in Poland
Autorzy:
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/2066019.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ropa naftowa
zagłębie
Polska
petroleum provinces
basin analysis
petroleum play
Polska
Opis:
The scheme in which the Carpathians, Carpathian Foredeep and Polish Lowland are distinguished as the hydrocarbon prospective zones was used hitherto in Poland. Good geological diagnosis of Poland area enables to distinguish the petroleum provinces in terms of basin analysis (methodology). This procedure are based on an integration of multidisciplinary geological and geophysical data with into a petroleum play concept. Results of drillings and petroleum play procedures allow to predict boundaries of petroleum provinces. Effects of basin analysis with regards to the stratigraphy of hydrocarbon-bearing areas are presented in Figure 1. All these prospective areas (Fig. 1) have been matched into five independent units (Fig. 2) which could be defined as following petroleum provinces: Pomerania, Wielkopolska, Ma3opolska, Lublin and Gdansk. These petroleum provinces are only the parts of sedimentary basins the individual development of which enabled generation, migration and preservation of hydrocarbons. Location of the above mentioned petroleum provinces is also brightly reflected on the map of crustal consolidation (Fig. 3): every province in Poland has its own individual geologic history.
Źródło:
Przegląd Geologiczny; 2007, 55, 12/1; 1061-1067
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Regionalizacja tektoniczna Polski-Niż Polski
Tectonic subdivision of Poland: Polish Lowlands
Autorzy:
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/2074565.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
regionalizacja tektoniczna
geologia regionalna
Polska
Niż Polski
niecka Polska
tektonika
podłoże
regional subdivision
regional geology
Polska
Polish Lowlands
Polish Basin
tectonics
basement
Opis:
Presented paper is a contribution to discussion about the tectonic regionalization in Poland. The Polish Lowlands, located between the Baltic shore and the highlands of the southern and central Poland, is the area discussed here. In this region mainly the Quaternary and the Neogene deposits with thickness rarely over 300 m are exposed. On the sub-Cenozoic surface occur mainly Cretaceous, Jurassic and Triassic rocks. Structural forms of the Polish Lowlands are directly associated with the Permian-Mesozoic Polish Basin inverted at the beginning of Cenozoic time. It is worthwhile indicating here that not only the Polish Trough was inverted but also the distal part of this basin, distinguished now as the Fore-Sudetic Monocline. Subdivision of the Polish Lowlands into tectonic units on the sub-Cenozoic surface was shown on Fig. 1. In the mid-Polish area antyclinorium belts of north-west to south-east orientation are located. The basement of the Polish Basin is built of the pre-Permian deposits, tectonized during pre-Alpine phases. To analyze the geology of Poland in the sub-Permian architecture the proper tectonic map (Fig. 2) is required with only the units of first order marked. Debate on tectonics of Poland requires also a map of basement consolidation units (Fig. 3). Indispensable completion of the presented maps is a geological cross-section of the Polish Lowlands (Fig. 4). It is clear that tectonic regionalization of Poland (with special attention to the Polish Lowlands) should be demonstrated on the three basic maps here presented. Spatial (both horizontal and vertical) relations between tectonic units should be considered in the light of sedimentary basin analysis, i.e., searching processes and stages of the structural evolution which essentially contributed to the recent tectonic diversification in regional geology.
Źródło:
Przegląd Geologiczny; 2008, 56, 10; 895-903
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Permian Basin as a main exploration target in Poland
Autorzy:
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/2066015.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
polskie zagłębie permiańskie
pola naftowe i gazowe
ropa naftowa
Polish Permian Basin
oil and gas fields
petroleum play
Opis:
The Polish Permian Basin (PPB) is a part of the Southern Permian Basin in theWestern and the Central Europe. Results of burial and thermal analyses as well as a configuration of the Moho surface of the Polish Basin suggest the asymmetrical basin model. History of the Polish Basin reveals that the Late Permian and the Early Triassic periods represent the main rifting phase and its later development resulted from thermal relaxation. During the Late Triassic and the Jurassic time some cooling of rift heat field took place, but the turning point in thermal evolution of the Polish Basin was at the Jurassic/Cretaceous boundary when the south-western part of the Polish Basin was uplifted and intensively eroded. The knowledge on the Permian Basin in Poland is chiefly connected with petroleum exploration. The gas fields are located mainly in the Rotliegend reservoirs. The Zechstein deposits, overlying the Rotliegend, are also in the area of economic interest: hydrocarbons occurring in carbonate deposits of the Werra (Zechstein Limestone - Ca1 ) and Stassfurt (Main Dolomite - Ca2) cyclothems. Several tens gas fields have been hitherto discovered within the Rotliegend sandstones and the Zechstein limestones. Reservoirs are the clastic, terrestrial deposits of the Lower Permian and calcareous, biogenic carbonates of the Zechstein. Evaporates, mainly salts of the Werra cyclothem, are the regional sealing for the mentioned reservoirs. Natural gas accumulated in the Rotliegend sandstones and the Zechstein limestones is of the same origin: it was generated from organic matter occurred in the Carboniferous rocks and it migrated to higher places where it became concentrated within favourable structural or lithofacies conditions. High nitrogen content in the natural gas from the Polish Permian Basin is explained that nitrogen is generated from an organic matter within a sedimentary basin at higher temperatures than methane. Location of high helium concentration corresponds to the area of highest heat flow during the Late Permian, Triassic and Jurassic times, evidencing the Late Permian-Early Mesozoic rifting process. Numerous oil gas fields discovered in the Main Dolomite (Ca2) unit constitute it as one of the most important exploration target in the Polish Basin. It composes the closed hydrodynamic system sealed from the top and the bottom by evaporates. Both the source rocks and reservoirs are characteristic for this unit. Influence of the burial and thermal history of the Polish Basin on a petroleum play generation within the Main Dolomite unit is clearly visible. The previous and the present petroleum discoveries in the Polish Permian Basin, comparing to the other petroleum provinces in Poland, indicate it as a main exploration target.
Źródło:
Przegląd Geologiczny; 2007, 55, 12/1; 1003-1015
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Budowa geologiczna oraz geneza i ewolucja bloku Gorzowa
Geology, origin and evolution of the Gorzów Block
Autorzy:
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/2074804.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geologia regionalna
basen polski
Polska
geologia naftowa
tektonika
regional geology
Polish Basin
NW Poland
petroleum geology
tectonics
Opis:
From the beginning of geological investigations of the Polish Lowlands both the geological and the regional tectonic units were used simultaneously. The Szczecin-Gorzów Synclinorium should be distinguished in terms of tectono-structural rules. The Gorzów Block - as a geological unit - is defined on the basis of extent and differentiation of the Upper Cretaceous thickness or by distribution of local structures (mainly halotectonic and halokinetic ones) developed in the Zechstein-Mesozoic complex. Basement in the Gorzów Block area is uplifted in its consolidated part and also the top of Moho is elevated. Both uplifts are well correlated with the Permian-Mesozoic palaeogeothermal anomaly. The Gorzów Block incorporates also the north-western part of Wolsztyn Ridge which was active during the Permian-Mesozoic time. In the early Rotliegend time this area was characterized by volcanic activity. In the late Rotliegend it was a source for clastics deposited around the Wolsztyn Ridge. Also the carbonate platform facies of the Main Dolomite (Ca2) is associated with this uplifted area. The mentioned region is situated in the distal part of asymmetric, Polish rift basin. Development of basin analysis - as an interdisciplinary domain of the Earth Sciences - indicates the need of applying various geological units, adequate to the considering problem. Modern research methods in geology (computerization, GIS) enable the data bases creation for individual geological units necessary for study of their origin and evolution up to their present geological pattern.
Źródło:
Przegląd Geologiczny; 2010, 58, 8; 680-688
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Regionalizacja tektoniczna Polski a geologiczna baza danych PITAKA
Regional tectonic subdivision of Poland versus geological database PITAKA
Autorzy:
Oziembłowski, P.
Karnkowski, P. H.
Powiązania:
https://bibliotekanauki.pl/articles/2074563.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
regionalizacja tektoniczna
geologia regionalna
Polska
tektonika
stratygrafia
baza geologiczna
GIS
regional subdivision
regional geology
Polska
tectonics
stratigraphy
geological database
Opis:
Discussion on the tectonic regional subdivision of Poland is a good opportunity to show a range of geological information of each tectonic unit and to emphasize the necessity of improvement of geological tectonic classifications, application of which in the geological databases is essential for correct usage of data collected. A good example is a geological and geophysical database PITAKA developed in the Polish Oil and Gas Company from 1987. Actually the PITAKA database contains data from 3191 boreholes which drilled Permian and younger deposits and from 4555 boreholes pierced into the older rocks. This paper presents location of 2D and 3D seismic studies done in digital technology from its introduction in Poland in 1973. In the Polish Lowlands area the Fore-Sudetic Monocline is the best geologically recognized region. The Pomeranian Anticlinorium and the Szczecin-Gorzów Synclinorium are relatively well documented. Numerous boreholes and seismic sections in those areas are associated with intensity of exploration of raw material deposits such as hydrocarbons, coal, copper, zinc and lead, sulfur and salts. Until now the PITAKA database does not contain all drilling data from Poland but it is constantly extended and supplemented.
Źródło:
Przegląd Geologiczny; 2008, 56, 10; 936-938
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Krytyczne elementy systemów naftowych w basenach sedymentacyjnych Polski
Critical elements of petroleum systems in the sedimentary basins in Poland
Autorzy:
Karnkowski, P. H.
Matyasik, I.
Powiązania:
https://bibliotekanauki.pl/articles/2075523.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
system naftowy
basen sedymentacyjny
Polska
petroleum system
sedimentary basin
Polska
Opis:
Progress in geological, geophysical and drilling sciences during the past 30 years has introduced to hydrocarbon exploration the concept of petroleum system, understood as an analysis of the factors necessary forformation and preservation of oil and natural gas deposits. Thefinal evaluation ofpetroleum system is the product of allfactors involved in the formation of hydrocarbon accumulations, which must be preserved proper chronology of events in the geological space. Such interdependences build often synergistic or antagonistic configurations. These configurations are called critical elements of the petroleum system. Reliable and comprehensive analysis of critical elements ofpetroleum system in sedimentary basins in Poland lets identify potential new areas of hydrocarbon exploration. In this context, a particularly promising area is the petroleum system of the Pita Claystone Formation (central part of the Polish Rotliegend Basin) and deep “Carpathians” with their palaeo-mesozoic basement and deeper part of the Carpathian Foredeep.
Źródło:
Przegląd Geologiczny; 2016, 64, 9; 639--649
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Underground hydrocarbons storages in Poland: actual investments and prospects
Autorzy:
Karnkowski, P. H.
Czapowski, G.
Powiązania:
https://bibliotekanauki.pl/articles/2066020.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
podziemny magazyn
gaz
ropa naftowa
wyczerpane złoża
jaskinie solne
Polskie Przedsiębiorstwo Ropy Naftowej i Gazu
underground storage
gas
oil
exhausted deposits
salt caverns
Polish Oil and Gas Company
Opis:
Poland has the limited gas and oil resources. Main hydrocarbons supplies are delivered to Poland mostly from Russia by oil and gas pipelines. Very large length of these pipelines as well as the local considerable wearing of devices induces the necessity of reserves storage. Geological conditions in Poland and a considerable quantity of exhausted gas deposits enabling in nearest years to the construction of underground gas storages (UGS) suggest the new investments in this sector of petroleum industry. Capacity amount of present active UGS is 1.58 x 10exp.9 mexp.3 but after finalizing of storages their volume will achieve 2.8 x 10exp.9 mexp.3. Special attention is paid to the Wierzchowice UGS (the biggest one in Poland) and to caverns leaching within the Zechstein salts cavern underground gas storages (CUGS) Mogilno and Kosakowo. Reservoirs of cavern type (expensive under construction) are a very efficient, modern source of gas system supply, particularly in periods of the seasonal demand fluctuations for gas - a very high during the winter season in the central and the northern Europe. Only caverns in salts allow to store both the gas and the liquid hydrocarbons. Construction of the UGS refers mostly to exhausted gas fields, discovered and exploited by the Polish Oil and Gas Company. Experience and capital of the state company located it as a leader in Poland in the field of construction and exploitation of underground storages. Their construction has the minimum influence on the environment. Utilization of exhausted hydrocarbons deposits (often with the existing mining infrastructure) is not almost at all troublesome for a local population and the environment and it offers considerable practical and economic benefits. The economical boom in the oil and gas market during last years creates new challenges for construction and exploitation of hydrocarbons underground storages.
Źródło:
Przegląd Geologiczny; 2007, 55, 12/1; 1068-1073
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petroleum geology of the Polish part of the Baltic region - an overview
Autorzy:
Pikulski, L.
Karnkowski, P. H.
Wolnowski, T.
Powiązania:
https://bibliotekanauki.pl/articles/2059075.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Baltic Region
petroleum geology
shale gas
Opis:
The Polish part of the Baltic region is located within the contact zone between two large geological units: the Precambrian platform and the Paleozoic platform. It comprises the Polish sector of the southern Baltic Sea and the adjacent onshore part of Northern Poland (Western and Eastern Pomerania). The fundamental geological pattern is defined by the Teisseyre-Tornquist Zone, separating the East European Craton from the Paleozoic platform. As a result of exploration activity in the onshore Pomerania region, four oil fields in Cambrian sandstones, seven gas fields in Carboniferous sandstones, six gas fields in Rotliegend sandstones, and eleven oil fields within the Zechstein Main Dolomite horizon have been discovered. The petroleum play of the southern Baltic Sea region and adjacent areas must be considered separately for Eastern and Western Pomerania. In the Peribaltic Syneclise we can only take into consideration organic matter appearing in lower Paleozoic rocks but their geothermal history refers to the period from the Vendian up to the recent. The present extent of the "oil window" in the Upper Cambrian rocks is mainly restricted to the offshore area. Reservoir properties of the "gas window" Cambrian rocks are rather low due to intensive diagenetic processes. Acquisition of gas should be possible by processes of hydraulic stimulation (tight gas). Lower Paleozoic rocks rich in organic matter (Ordovician and Silurian), especially in the border zone of the EEC (Ro >>gt; 1.3%), could be an area of unconventional gas fields (shale gas). The Western Pomerania petroleum play shows two separate source rocks units. The older one embraces Carboniferous deposits with organic matter of terrestrial origin and generated gases accumulated in the Rotliegend and Carboniferous traps. The second petroleum system is located within the carbonates of the Zechstein Main Dolomite (Ca2). This is a closed system, meaning that the source rocks are at the same time the reservoirs sealed by Zechstein evaporates. Hitherto discovered hydrocarbon deposits in the Polish part of the Baltic region have confirmed good perspectives regarding oil and gas hydrocarbon zones. New, conventional and unconventional discoveries remain possible.
Źródło:
Geological Quarterly; 2010, 54, 2; 143-158
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-10 z 10

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