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2 2010

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Złoża węglowodorów w utworach cechsztyńskiego dolomitu głównego (Ca2) na bloku Gorzowa

Czekański E., Kwolek K., Mikołajewski Z.

Przegląd Geologiczny

2010

Vol. 58, nr 8

695-703

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.

Instalacja geotermalna w Pyrzycach jako przykład pozyskiwania czystej i odnawialnej energii w ciepłownictwie oraz wód termalnych do balneologii i rekreacji

Biernat H., Kulik S., Noga B.

Przegląd Geologiczny

2010

Vol. 58, nr 8

712-716

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.

Ewolucja górnopermskich (cechsztyńskich) basenów ewaporatowych w rejonie Gorzowa Wielkopolskiego (Zachodnia Polska)

Czapowski Grzegorz, Małolepszy Zbigniew, Szynkaruk Ewa, Chełmiński Jacek, Nowacki Łukasz

Przegląd Solny

2021/2022

T. 16

163--167