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Tytuł:
Metan pokładów węgla: zasoby i eksploatacja
Coalbed methane: resources and recovery
Autorzy:
Hadro, J.
Wójcik, I.
Powiązania:
https://bibliotekanauki.pl/articles/2075077.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
coalbed methane (CBM)
CBM
coal mine methane CMM
CMM
CBM resource
CBM reserves
CBM production
metan pokładów węgla
metan kopalniany
zasoby CBM
rezerwy CBM
produkcja CBM
Opis:
Gas produced from coal can be subdivided into three categories: coalbed methane (CBM), coal mine methane (CMM) and abandoned mine methane (AMM). CBM is extracted from virgin coal using wells drilled from the surface. In recent years horizontal drilling is widely used as a primary CBM recovery technique. A pair of wells - a vertical production well intersected by a horizontal multilateral well - is considered the most effective in dewatering a coal reservoir and thus enables maximizing its productivity. Although CBM world resources are huge (100-216 bcm), only a few countries produce coalbed gas commercially. While the US is still the leader, Australia has the fastest CBM production growth. It has been observed that many mature CBM plays reveal highly variable productivity, possibly due to coal heterogeneity. Therefore, CBM reserves/resources should be estimated using probabilistic methods. In spite of its substantial CBM resource potential, Poland has produced only coal mine methane (CMM) whereas significant efforts of CBM exploration conducted in the 1990s failed to flow gas in commercial quantities due to low permeability. Dart Energy operates a CBM exploration license in the Upper Silesia and has recently finished testing the CBM production pilot using a surface-to-inseam horizontal well with vertical production well intersection. This state-of-the-art CBM completion technology has been used for the first time in Poland and, hopefully, will unlock the sizeable CBM resource of the Upper Silesian Coal Basin.
Źródło:
Przegląd Geologiczny; 2013, 61, 7; 404--410
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geologiczna i geomorfologiczna interpretacja danych z lotniczego skaningu laserowego (ALS) rejonu KasprowegoWierchu (Tatry) – odpowiedź
Autorzy:
Wojciechowski, T.
Wójcik, A.
Perski, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2066629.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
lotniczy skaning laserowy
ALS
Kasprowy Wierch
Źródło:
Przegląd Geologiczny; 2014, 62, 2; 83--85
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Porównanie właściwości ekspansywnych iłów neogeńskich z Mazowsza
Comparison of expansive properties of Neogene clays from the Mazovia region
Autorzy:
Gawriuczenkow, I.
Wójcik, E.
Powiązania:
https://bibliotekanauki.pl/articles/2075056.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
expansion
Neogene (Mio-Pliocene) clay
swelling pressure
mineral composition
clay fraction
ekspansywność
iły neogeńskie
ciśnienie pęcznienia
skład mineralny
zawartość frakcji iłowej
Opis:
Development of building projects in the Mazovia region causes the risk of their location on the soils of specific expansive properties. These properties, expressed as swelling or shrinkage, are a serious engineering problem. Many methods are used for the evaluation ofexpansiveness; both direct and indirect test methods are used. Tests were performed on clays from the areas of Warsaw, Dobre near Mińsk Mazowiecki and Mszczonów. Comparative analysis of expansive properties of Neogene clays is based on the results of laboratory tests of mineral composition, grain size distribution, moisture content, free swelling and swelling pressure. The tests have shown that the expansive properties ofclays from the Mazowsze region can have extremely high values, which causes the needfor individual determination of potential expan-siveness for different types of clays, depending on moisture content, swelling pressure and chemistry of the environment.
Źródło:
Przegląd Geologiczny; 2013, 61, 4; 243--247
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wałbrzyskie hałdy i osadniki kopalniane jako źródło surowców wtórnych - wstępne wyniki inwentaryzacji
Wałbrzych mine waste dumps and sedimentation ponds as secondary raw materials sources - preliminary results of the survey
Autorzy:
Wójcik, J.
Powiązania:
https://bibliotekanauki.pl/articles/2074938.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kopalniane hałdy
osadniki
odpady
antropogeniczne złoża
mine waste dumps
sedimentation tanks
wastes
anthropogenic deposits
Opis:
The development of coal mining and power industry contributed to the accumulation of significant quantities of mining and processing wastes on the land surface in Wałbrzych and Boguszów Gorce. The main components of the mine waste dumps are gangues rocks and in smaller quantities: post-flotation waste and slag and ashes. Approximately 85 million cubic meters of such waste are disposed on the dumps with a volume over 1 million cubic meters. Approximately 3.4 million cubic meters of coal sludge and ashes remains in the bowls of former sedimentation tanks. The majority of the waste (81%) is located in the area of Wałbrzych. In the years 1975–1996, only approx. 1% of the waste from the mine waste dumps and sedimentation tanks was used for various purposes. Significant amounts of the waste accumulated on the land surface can be considered as prospective anthropogenic deposits. This is indicated by the attempts made so far to use them as secondary raw materials as well as by few studies providing the information for what purposes the waste can be used. It is therefore necessary to carry out detailed identification works on the quality and quantity of the deposited wastes, what is a prerequisite for the optimal use of these wastes in the future.
Źródło:
Przegląd Geologiczny; 2012, 60, 4; 212-219
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Strukturalne uwarunkowania rzeźby Wyżyny Lubelskiej i Roztocza
Structural control on the relief in the Lublin Upland and the Roztocze region
Autorzy:
Dobrowolski, R.
Harasimiuk, M.
Brzezińska-Wójcik, T.
Powiązania:
https://bibliotekanauki.pl/articles/2075098.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
structural morphology
structure of Upper Cretaceous rock massif
neotectonics
Lublin Upland
Roztocze region
struktura morfologiczna
skalne stryuktury dolnokredowe
masyw górski
neotektonika
Wyżyna Lubelska
Roztocze
Opis:
The main relief features of the Lublin Upland (sensu Jahn, 1956) and Roztocze were formed during the early and middle Cenozoic stages of the Meta-Carpathian Ridge morphogenesis. They are clearly conditioned by the structure of the Upper Cretaceous-Palaeogene complex of the marginal part of the East European Craton. The following factors were of fundamental significance for the relief development in the study area: 1) Alpine and modern tectonic activity, which conditioned the horst nature of some morphostructures and the type of fissuring of rock massif, and 2) lithological diversity of the Upper Cretaceous-Palaeogene complex as well as the Miocene and Pliocene deposits, which influenced its strength features.
Źródło:
Przegląd Geologiczny; 2014, 62, 1; 51--56
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rozpoznanie i próby zabezpieczenia osuwiska w Kurowie (Pogórze Rożnowskie, Karpaty Zewnętrzne)
Recognition and attempts for the Kurów landslide protection (Rożnów Foothills, Outer Carpathian)
Autorzy:
Wójcik, A.
Kos, J.
Jurczak, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075677.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ruchy masowe
osuwisko w Kurowie
ochrona osuwisk
Karpaty fliszowe
południowa Polska
mass movements
Kurów landslide
landslide protection procedure
flysch Carpathians
southern Poland
Opis:
In 2010-2015, various research teams conducted geological operations on the Kurów landslide. They independently documented the course of deep-seated slip surfaces. The studies were carried out in three stages, embracing preparation of expert’s reports, geological documentation, and reports on monitoring work. The procedures used in Małopolska, worked out within the framework of the SOPO (LCS-Landslide Counteracting System) project, were of great importance during the recognition and protection ofpart of the landslide area. It was proposed that the scope (depth and distribution of boreholes) have been consulted with the appropriate representative of the scientific surveillance of the PGI-NRI Carpathian Branch in Cracow before the tendering procedure.
Źródło:
Przegląd Geologiczny; 2017, 65, 9; 576--585
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wstępne wyniki badań petrologicznych i palinologicznych klastów węgla w zlepieńcach formacji menilitowej jednostki śląskiej
Preliminary petrological and palinological characteristics of coal clasts from the Menilite Formation of the Silesian Unit
Autorzy:
Wójcik-Tabol, Patrycja
Górecka-Nowak, Anna
Nowak, Grzegorz
Powiązania:
https://bibliotekanauki.pl/articles/2075964.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
konglomerat węglowy
vitrinit
liptinit
inertyn
palinofacje
miospory
coal-bearing conglomerate
vitrinite
liptinite
inertinite
palynofacies
miospores
Opis:
Coal-bearing conglomerates occur in the Menilite Formation of the Silesian Unit, outcropped in the village of Kobielnik. Coal particles are angular and differ in size (2 mm-6 cm). The examined coal shows rather predominance of vitrinite (collotelinite, collodetrinite, vitrodetrinite). However, the presence of inertinite (fusinite, semifusinite and inertodetrinite with rather accessory funginite and secretinite) is also significant. However, liptinite (sporinite, cutinite and resinite) also indicates its presence in the maceral composition. The results of both coal petrographic and palynologcal analyses were conducted with the intention of applying them to reconstruct environments of coalformation. Palynological studies revealed palynofacies consisting mainly of black palynoclasts ofrectangle or oval shape. Miospores are abundant and various in colour-from yellow to dark brown. The miospore assemblage is dominated by Lycospora and several other Carboniferous genera occur there. The presence of Radiizonates aligerens (Knox) Staplin, Jansonius, the guide species to the lower part of the Westphalian A (Langsettian) indicate that at least part of the coal pieces come from this part of the Pennsylvanian. The age position of the whole miospore assemblage should be determined as the Late Bashkirian-Moscovian (Westphalian). Additionaly, some older miospores, usually dark in colour, were found in this assemblage and they are considered as reworked.
Źródło:
Przegląd Geologiczny; 2019, 67; 200--203
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Morena szaflarska w świetle nowych danych z odsłonięć i wierceń w 100-lecie jej odkrycia
Szaflary moraine in the light of new data from exposures and drilling on the 100th anniversary of its discovery
Autorzy:
Wójcik, Antoni
Powiązania:
https://bibliotekanauki.pl/articles/2087064.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Czwartorzęd
Podhale
tatrzańskie lodowce
morena
kamieniołom w Szaflarach
Quaternary
Podhale Region
Tatra glaciers
moraine
quarry in Szaflary
Opis:
In the northern part of the Podhale Region, nearly 100 years ago, Matkowski (1924, 1928) described gravels exposed in a quarry in Szaflary and considered them to be moraine sediments - Szaflar moraine. Romer (1929) confirmed this interpretation of the sediments. Later studies of Halicki (1930), Klimaszewski (1948, 1988), Birkenmajer (1976) and Birkenmajer and Stuchlik (1975) completely excluded the possibility of moraines in this area and showed that these sediments have are of fluvioglacial origin. Comparing the quarry's ranges due to exploitation, it was found that the authors could observe various deposits exposed during the progress of exploitation towards the west. In the profiles of trenches for new buildings to the NW from the quarry, clays containing sands and gravels and individual boulders and blocks of quartzite and granite with a diameterof0.8 to 1.2m were found. The exposed erratics exactly correspond to the description of the moraine by Matkowski (1924, 1928) from the quarry in Szaflary. In addition, in the recently drilled Nowy Targ PIG-2 borehole, similarly developed pieces were found at a depth of19.7-69.5 m. Combining archival data and new facts from drilling and exposures, a view can be proposed that, during the Southern Polish Glaciations, the Tatra glaciers reached the Nowy Targ Basin and perhaps the foothills of the Gorce Mts, which was already suggested by Rehman (1895), Zapatowicz (1913) and Matkowski (1928).
Źródło:
Przegląd Geologiczny; 2022, 70, 6; 458--467
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie numerycznych obliczeń stateczności zboczy dla oceny potencjalnych stref przemieszczeń zwietrzelin i koluwiów rozwiniętych na podłożu fliszowym
Application of slope stability numerical calculation for evaluation of potential displacement zones in weathered and colluvial soils on the flysh base
Autorzy:
Dobak, P.
Gawriuczenkow, I.
Kaczmarek, Ł. D.
Kiełbasiński, K.
Wójcik, E.
Powiązania:
https://bibliotekanauki.pl/articles/2075539.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
zbocze
stateczność
modelowanie numeryczne
materiałowy model multilaminate
zwietrzelina
development of slope
stability
numerical modeling
multilaminate material model
weathering
Opis:
This study concerns the modeling potential of slopes development with use of numerical stability calculations. Boundary conditions of performed numerical simulations are according to morphological and geological engineering conditions of the flysch slope shaped by weathering and surface mass movements. The multilaminate material model was used in order to imitate shale spatial variation in weathering zones. Furthermore, X-ray computed microtomography technique enabled for visualization of varied condition of shear surface extortion, which cause physical and strength parameters diversity. Calculation outputs show that geometry and location of deformation zones are affected by a model input strength parameter. The presented results confirm utility of numerical modeling as important aspect in the investigation and verification of spatiotemporal slope development cycle.
Źródło:
Przegląd Geologiczny; 2016, 64, 9; 683--693
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ropa naftowa i gaz ziemny w Polsce : obszary perspektywiczne oraz postępowanie przetargowe w 2018 r. (część I)
Oil and gas in Poland : prospects and licensing rounds in 2018 in terms of hydrocarbon concessions (part I)
Autorzy:
Jagielski, G.
Feldman-Olszewska, A.
Janas, M.
Kiersnowski, H.
Krzyżak, E.
Podhalańska, T.
Roszkowska-Remin, J.
Sobień, K.
Wójcik, K.
Powiązania:
https://bibliotekanauki.pl/articles/2075843.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
koncesje na poszukiwanie
rozpoznawanie węglowodorów
eksploatacja węglowodorów
Ministerstwo Środowiska
concessions for prospection
exploration of hydrocarbons
exploitation of hydrocarbons
Polish Ministry of the Environment
Opis:
On the 28th of June 2017, the Polish Ministry of the Environment announced the boundaries of the tender areas selected for the third licensing round for concessions for prospection, exploration and exploitation of hydrocarbons. This round is going to be proceeded in the 4th Quarter of 2018 and 1st Quarter of 2019. The geologists of the Polish Geological Survey selected 15 tender areas (promising for discoveries of conventional and unconventional oil and gas fields) based on the geological data resources stored in the National Geological Archive, other published data, as well as the knowledge and experience of employees of the Polish Geological Institute - National Research Institute and the Polish Ministry of the Environment. All selected areas are located onshore. In this article we describe 10 tender areas located in the Gdańsk, Pomerania and Wielkopolska petroleum provinces. Other tender areas situated in the Carpathians (Błażowa, Proszowice W, Rudnik-Lipiny, Wetlina) and in the Lublin Petroleum Province (Ryki) will be discussed in the next publication. Three areas: Wejherowo, Bytów and Braniewo-Miłakowo are located in the northern Poland (Gdańsk Petroleum Province). The exploration targets of these areas are generally related to structural-lithological traps in the Middle Cambrian beds of the Baltic Basin, as well as to unconventional shale oil and gas in the Lower Paleozoic. Seven tender areas are situated in the northwestern Poland (Pomerania and Wielkopolska Petroleum Provinces). Three of them - Chodzież, Piła and Leszno are dedicated to conventional gas deposits in the Rotliegend sandstones and, in some cases, also oil deposits in the Zechstein/Main Dolomite. Excluding the Leszno tender area, chances for tight gas discoveries exist within the Rotliegend sandstones. The exploration target of the Konin tender area is related to possible conventional fields in the Jurassic and Lower Cretaceous beds. In the Pomerania region the exploration target is generally related to conventional hydrocarbon deposits in the Devonian, Carboniferous and Permian (Rotliegend and Zechstein/Main Dolomite). Three tender areas are situated within the region of: Sierpowo, Orle and Chełmno. As a rule, a concession is granted for a period of 10 to 30 years and is divided into 2 phases: 1) prospecting and exploration phase (which lasts from 4 to 5 years and can be extended to another 2-year period), 2) production phase. 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 encourage activity in the Polish oil and gas sector.
Źródło:
Przegląd Geologiczny; 2018, 66, 12; 724--740
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ropa naftowa i gaz ziemny w Polsce – obszary perspektywiczne oraz postępowanie przetargowe w 2018/2019 r.
Oil and gas in Poland - prospects and licensing rounds in 2018/2019 in terms of hydrocarbon concessions (part II)
Autorzy:
Feldman-Olszewska, Anna
Jankowski, Leszek
Krzyżak, Ewelina
Peryt, Tadeusz
Sikorska-Jaworowska, Magdalena
Wójcik, Krystian
Powiązania:
https://bibliotekanauki.pl/articles/2075891.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
obszary przetargowe
Lubelskie województwo ropopochodne
Małopolska
ropa naftowa i gaz
złoża węglowodorów
tender areas
Lublin and Małopolska Petroleum Provinces
oil and gas
hydrocarbon deposits
Opis:
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.
Źródło:
Przegląd Geologiczny; 2019, 67, 1; 13--26
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Poszukiwanie i rozpoznawanie złóż ropy naftowej i gazu ziemnego w Polsce : szósta runda przetargowa
Prospection and exploration of oil and gas fields in Poland : 6th tender round
Autorzy:
Wójcik, Krystian
Zacharski, Jarosław
Łojek, Marcin
Wróblewska, Sara
Kiersnowski, Hubert
Waśkiewicz, Krzysztof
Wójcicki, Adam
Laskowicz, Rafał
Sobień, Katarzyna
Peryt, Tadeusz
Chylińska-Macios, Agnieszka
Sienkiewicz, Jagoda
Powiązania:
https://bibliotekanauki.pl/articles/2087054.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ropa naftowa
gaz ziemny
poszukiwania ropy
obszary przetargowe
polityka otwartych drzwi
crude oil
natural gas
petroleum prospective
tender areas
open door policy
Opis:
On June 30, 2021 the Polish Minister of Climate and Environment announced the boundaries of five areas dedicated for the next, 6th tender round for hydrocarbon concessions in Poland, planned for the second half of 2022. These are: Block 413-414, Block 208, Cybinka-Torzym, Zielona Góra West, and Koto tender areas. The main exploration target of these areas is related to conventional and unconventional accumulations of gas and oil in the Carpathian basement, Carpathian Foredeep and Outer Carpathians (Block 413-414), as well as in the Carboniferous, Permian Rotliegend, Zechstein Limestone, and Main Dolomite (Block 208, Cybinka-Torzym, Zielona Góra West) and in the Mesozoic of the Polish Lowlands (Koto). The other way of granting hydrocarbon concessions in Poland is the open door procedure, in which an entity may apply for concessions for any other area.
Źródło:
Przegląd Geologiczny; 2022, 70, 5; 363--372
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Koncesje na poszukiwanie, rozpoznawanie oraz wydobywanie złóż ropy naftowej i gazu ziemnego w Polsce w 2019 i 2020 roku : postępowanie przetargowe i przetarg inwestorski
Prospection, exploration and production of hydrocarbons in Poland in 2019 and 2020 : tender procedure vs open door policy
Autorzy:
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
Powiązania:
https://bibliotekanauki.pl/articles/2075919.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
olej
gaz
koncesje węglowodorowe
postępowanie przetargowe
przetarg inwestorski
oil
gas
hydrocarbon concessions
tender areas
open door policy
Opis:
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.
Źródło:
Przegląd Geologiczny; 2019, 67, 12; 938--960
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geologiczna i geomorfologiczna interpretacja danych z lotniczego skaningu laserowego (ALS) rejonu Kasprowego Wierchu (Tatry)
Geological and geomorphological interpretation of Airborne Laser Scanning (ALS) data of the Kasprowy Wierch area (Tatra Mts.)
Autorzy:
Wójcik, A.
Wężyk, P.
Wojciechowski, T.
Perski, Z.
Maczuga, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075057.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Airborne Laser Scanning
digital terrain model (DTM)
Tatra Mts.
Kasprowy Wierch Mt.
Goryczkowa Valley
lotniczy skaning laserowy (ALS)
ALS
cyfrowy model terenu
Tatry
Kasprowy Wierch
Dolina Goryczkowa
Opis:
The paper presents the geological interpretation of Airborne Laser Scanning data of Kasprowy Wierch Mt. area. The analyzed points cloud data represent the ground surface after removal of the land cover (primarily vegetation) objects. The ALS data were characterized by very high density, presenting even minor terrain forms, very difficult to identify in forested and mountain dwarfpine areas as well. The resulting image of detailed geomorphology of the study area was compared with existing maps at scale of 1 : 10 000 and literature data. This allowed verifying the extent of geological units of basement rocks and shed new light on existing opinions on the genesis of glacial sediments. An extensive landslide has been identified on the eastern slopes of Sucha Czuba Mt. The landslide has not been reported in the literature so far. Application of laser scanning data was extremely useful and allowed making new observations that enrich the existing knowledge about the geology of this part of the Tatra Mts.
Źródło:
Przegląd Geologiczny; 2013, 61, 4; 234--242
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena możliwości zastosowania metody georadarowej i elektrooporowej do identyfikacji rozluźnionych stref gruntów niespoistych
Evaluation of the applicability of GPR and resistivity methods for identifying loose zones in non-cohesive soils
Autorzy:
Mieszkowski, R.
Zawrzykraj, P.
Żmudzin, D.
Wójcik, E.
Popielski, P.
Powiązania:
https://bibliotekanauki.pl/articles/2075707.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
metoda georadarowa
GPR
metoda elektrooporowa
ERT
sondowanie dynamiczne
DPL
zagęszczenie nasypu
wskaźnik zagęszczenia
ground penetrating radar method
electrical resistivity tomography method
dynamic sounding
relative density
degree of compaction
Opis:
The results of the possibility of geophysical methods application (such as geoelectrical ones, including ground penetrating radar and electrical resistivity tomography) to identify areas of loose sands were presented in the article. Registered anomalies obtained from geophysical survey have been verified by geological and engineering tests (drillings and dynamic probing). Measurements were carried out along the part of the lateral earth dam, consisting of man-made soils with a thickness of approximately 7 m and underlying alluvial medium grained sands. The results obtained from the geophysical survey and direct assessment of density by means of dynamic probing allowed to demonstrate the relationship between a specific type of geophysical anomalies and the density of non-cohesive man-made soils.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/2; 779--784
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 16

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