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3 2019

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Ropa naftowa i gaz ziemny w Polsce – obszary perspektywiczne oraz postępowanie przetargowe w 2018/2019 r.

Feldman-Olszewska Anna, Jankowski Leszek, Krzyżak Ewelina, Peryt Tadeusz, Sikorska-Jaworowska Magdalena, Wójcik Krystian

Przegląd Geologiczny

2019

Vol. 67, nr 1

13--26

On the 28th of June 2017, the Polish Ministry of the Environment announced the boundaries of the 15 tender areas selected for the third licensing concession round for prospection, exploration and exploitation of hydrocarbons. In this paper we describe the areas located in the south-eastern (Ryki) and southern Poland (Proszowice W, Rudnik-Lipiny, Błażowa and Wetlina). The other areas have already been described in the previous issue of the Przegląd Geologiczny. The exploration target of the Ryki area is related to conventional gas deposits in the Upper Devonian and Carboniferous, as well as to unconventional tight gas deposits in the Frasnian carbonates. Prospects in the tender areas located in southern Poland are related to conventional oil and gas deposits in the Carpathians, Carpathian Foredeep and their Paleozoic-Mesozoic basement.

Koncesje na poszukiwanie, rozpoznawanie oraz wydobywanie złóż ropy naftowej i gazu ziemnego w Polsce w 2019 i 2020 roku : postępowanie przetargowe i przetarg inwestorski

Jagielski Grzegorz, Jankowski Leszek, Kiersnowski Hubert, Kijewska Sylwia, Kozłowska Aleksandra, Krzyżak Ewelina, Kuberska Marta, Laskowicz Rafał, Rosowiecka Olga, Roszkowska-Remin Joanna, Smajdor Łukasz, Wesołowski Marcin, Wójcik Krystian, Żuk Tomasz

Przegląd Geologiczny

2019

Vol. 67, nr 12

938--960

A concession for prospection, exploration and production of hydrocarbons from deposits or a concession for production of hydrocarbons from deposits shall be granted by the way of a tender procedure or at the request of the interested entity. On June 28, 2018 the Polish Minister of the Environment announced the boundaries of the five tender areas dedicated for the next, 4th tender round for hydrocarbon concessions in Poland. These are: Bestwina-Czechowice, Królówka, Pyrzyce, Złoczew and Żabowo. The main exploration target of the areas located in southern Poland (Carpathians) - Bestwina-Czechowice and Królówka - is related to conventional accumulations of gas in the Miocene of the Carpathian Foredeep and to conventional and unconventional accumulations of gas and oil in the Paleozoic-Mesozoic basement of the Carpathian units. On the other side, the conventional accumulations of gas in the Permian Rotliegend sandstones and conventional and unconventional accumulations of gas and oil in the Zechstein/Main Dolomite carbonates are expected in the Pyrzyce, Żabowo and Złoczew areas, in central and north-western Poland. The beginning of the tender is planned for Q1 2020. The tender will last 180 days. The entities can also apply for a concession submitting an application to the Licensing Authority . However, the area indicated by the entity cannot be a subject of a tender or any other concession, and the maximum acreage cannot exceed 1200 km2. As a rule, a concession is granted for a period of 30 years and will be divided into 2 phases: (1) prospection and exploration phase (which lasts no longer than 5 years, but in justified cases can be extended), (2) production phase (25 years). Every entity interested in obtaining a concession needs to undergo the qualification procedure. We believe that this publication will contribute to better understanding of the offered tender areas and boosts the activity in the Polish oil and gas sector.

Occurrence of clastic injectites in the Oligocene strata of the Carpathians and their significance in unravelling the Paleogene and Neogene evolution of the Carpathian orogeny (Poland, Ukraine and Romania)

Jankowski Leszek, Wysocka Anna

Geological Quarterly

2019

Vol. 63, No. 1

106--125

The irregular distribution of sand injections, traditionally termed “dykes” in the Polish geological literature, within individual Carpathian units and within individual lithofacies were observed during long-lasting field works. Injectites have been observed in the Magura Beds and in the Inoceramian Beds of the Polish and Romanian Carpathians, and in the Central Carpathian Paleogene deposits. However, they are most common in the Oligocene-Miocene Menilite Beds, where they are typical and abundant, particularly in the Skole Unit. Two clastic injectite types were distinguished: sedimentary (S-type) and tectonized (T-type). Based on the occurrence and interpretation of these injectites a new two-stage conceptual model is proposed for the Polish segment of the progressive Oligocene-Miocene Carpathian orogenic belt evolution. Type S clastic injectites are interpreted as having formed in the compressional stage, during foredeep basin migration while depositional slope changes were taking place in the Late Oligocene to Early Miocene. Type T injectites are interpreted as having formed by reactivation of S-type injectites in the last, mainly strike-slip, phases of Carpathian orogenic belt formation.