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    Wyświetlanie 1-5 z 5
    Tytuł:
    Złoża węglowodorów w utworach cechsztyńskiego dolomitu głównego (Ca2) na bloku Gorzowa
    Hydrocarbon fields in the Zechstein Main Dolomite (Ca2) on the Gorzów Block (NW Poland)
    Autorzy:
    Czekański, E.
    Kwolek, K.
    Mikołajewski, Z.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074806.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    cechsztyński dolomit główny
    blok Gorzowa
    złoża ropy naftowej i gazu ziemnego
    Zechstein Main Dolomite
    Gorzów Block
    oil and gas fields
    Opis:
    By discoveries of hydrocarbon deposits in the Polish part of the Southern Permian Basin, Western Poland became a key explorational area. The most spectacular discoveries have been done on the Gorzów Block which borders the Fore-Sudetic Monocline from the south and the Szczecin Swell from the north. This is the area where the biggest oil field - Barnówko-Mostno-Buszewo (BMB) - have been discovered and the group of oil and gas deposits Lubiatów-Międzychód-Grotów (LMG). Detailed litho- facies analysis of Main Dolomite carbonates and seismic surveys (mainly 3D) contributed to good recognition of depositional architecture in this part of the Main Dolomite basin. An interesting issue is the relationship of the discovered deposits with carbonate depositional zones and diverse chemical composition of hydrocarbons. Most of deposits is related to carbonate platforms and microplatforms. Less important are platform slopes but basinal zone is and was considered as the area where source rocks occur. Discovery of the Lubiatów oil deposit at the foot of the Grotów Peninsula opened new possibilities in searching for hydrocarbons. Later negative results of drillings in this zone did not affected the fact that there are still explorational hopes for this type of carbonates. Hydrocarbons which can still be discovered in this interval are still not known based on calculations done in the recent years. It seems, that better geochemical recognition and advanced look on diagenetic evolution and depositional architecture will bring about new discoveries in the Main Dolomite interval on the Gorzów Block.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 8; 695-703
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Szczątki nosorożca (Stephanorhinus sp.) oraz daniela (Dama dama) odkryte w osadach kopalnego jeziora eemskiego na Równinie Gorzowskiej
    Remains of rhinoceros (Stephanorhinus sp.) and fallowdeer (Dama dama) discovered in Eemian lake sediments in the Gorzów Plain (NW Poland).
    Autorzy:
    Badura, J.
    Ciszek, D.
    Kotowski, A.
    Przybylski, B.
    Ratajczak, U.
    Stefaniak, K.
    Urbański, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075742.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    nosorożec
    fauna plejstoceńska
    zlodowacenie eemskie
    Gorzów Wielkopolski
    NW Polska
    Rhinocerotidae
    Pleistocene fauna
    Eemian Interglacial
    NW Poland
    Opis:
    Erthwork during rebuilding of the S3 route in Gorzów Wielkopolski exposed sediments of a palaeolake. The thickness of the sediment complex reaches 11 m. Two gyttja layers are separated by peats and fluvial sands and muds. The sequence reflects a multiphase development of the lake. Lacustrine sediments overlie Odranian (Saalian) (MOIS 6) glaciofluvial deposits and are covered by Vistulian glacial sediments (MOIS 2). At present, the stratigraphic position of the palaeolake is dated to the Eemian (MOIS 5e), with a probable continuation of the deposition into the early Vistulian (MOIS 5d-4). Rhinoceros bones (more than 100 pieces), including a skull with 24 well-preserved teeth, were discovered in the lower part of the palaeolake sediments. The preliminary expertise report, based mainly on the teeth analysis, allows assigning the rhinoceros remains into the genus Stephanorhinus. The finding of so many pieces of the skeleton of Stephanorhinus sp. in situ is unique on the scale of European scale. Apart from the rhinoceros remains, a single metacarpal bone of fallow deer (Dama dama) was found in the site. This is the first record of extant fallow deer in the Pleistocene of Poland. The palaeolake sediments were sampled and multidisciplinary research is planned to reconstruct the history of the development of this basin. The relationship between the rhinoceros andfallow deer remains with the palaeoenvironment will make it possible to ascertain the conditions in which those animals lived at higher latitudes during the Eemian Interglacial.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 4; 219--226
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ewaporaty cechsztynu PZ1- PZ3 bloku Gorzowa
    Zechstein 1- 3 evaporites of the Gorzów Block (NW Poland)
    Autorzy:
    Peryt, T. M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074802.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    cechsztyn
    ewaporaty
    stratygrafia sekwencji
    Polska Zachodnia
    Zechstein
    evaporites
    sequence stratigraphy
    West Poland
    Opis:
    The Gorzów Block (West Poland) occurs in the transition zone between the PZ1 sulphate platform and the Na2 basin. In contrast to the western part of the Southern Permian Basin where the Z1 halite (Oldest Halite Na1) is normally restricted to the peripheral subbasins located south of the main basin, in Poland it occurs both in the basin centre and in the former basins of the Lower Anhydrite within the marginal sulphate platform complex, where halite sequences are thick and may have originated in a deep-water setting. The Na1 deposits have been considered so far to be LST deposits both in the marginal sulphate platform facies as well as in the basin centre. Brine salinities (and the minerals they precipitate) are controlled by brine residence times in the basin, and these are determined primarily by the absolute and the relative rates of water flow into, and brine flux out of the basin (Kendall, 2010). Thus sea-level rise in the Boreal Sea could have resulted in the increase of the brine residence times in the Zechstein basin and the deposition of more saline evaporites. Consequently, the Oldest Halite in the basin centre in Poland is regarded as the TST deposit.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 8; 689-694
    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:
    Instalacja geotermalna w Pyrzycach jako przykład pozyskiwania czystej i odnawialnej energii w ciepłownictwie oraz wód termalnych do balneologii i rekreacji
    Geothermal heating plant in Pyrzyce (NW Poland) as an example of sourcing of thermal energy and waters for balneology and recreation
    Autorzy:
    Biernat, H.
    Kulik, S.
    Noga, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074805.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    energia geotermalna
    region Pyrzyc
    Polska
    geothermal energy
    Gorzów Block
    NW Poland
    Opis:
    Thermal waters (61°C) occurring in the Lower Jurassic reservoirs in the Pyrzyce region (approx. 1600 m b.s.l.) are used mainly in heating plant and their chemical composition allow to apply them in balneology and recreation. In the summer time in the Pyrzyce plant only the geothermal waters are used. In the autumn-winter season, when higher temperatures of water for municipal network are needed, the system is supported by absorption heat pumps. Usage of geothermal waters in the Pyrzyce municipal heat system eliminated small carbon boilers and reduced considerable emission of harmful substance to atmosphere.
    Źródło:
    Przegląd Geologiczny; 2010, 58, 8; 712-716
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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