Autor: Peryt, Tadeusz - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Stulecie Polskiego Towarzystwa Geologicznego
On the centenary of the Polish Geological Society
Autorzy:: Peryt, Tadeusz Marek
Powiązania:: https://bibliotekanauki.pl/articles/20204494.pdf
Data publikacji:: 2022
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: towarzystwa geologiczne
ASGP
Stypendium im. Krzysztofa Beresa
Nagroda im. Ludwika Zejsznera
Nagroda Henryka Świdzińskiego
geological societies
Krzysztof Beres Scholarship
Ludwik Zejszner Prize
Henryk Świdziński Prize
Opis:: In 2021, when the very respected Polish Geological Society celebrated its centenary, a number of jubilee events were organized in online format, but because of Covid-19 pandemic the ceremonial jubilee session was postponed to May 18, 2022, and the Auditorium Maximum of the Jagiellonian University in Cracow was chosen for this event. President of Republic of Poland Andrzej Duda took National Patronage over the event. The main forms of the Society's activity since its beginning have been scientific meetings, annual conferences organized in various parts of Poland, and the publication of the journal Annales Societatis Geologorum Poloniae. The Society also organizes the Polish geological congresses (every four years) and meetings of international societies and associations; all of them have appeared very successful in terms of the number of participants and the impact for development of geological sciences.
Źródło:: Przegląd Geologiczny; 2022, 70, 4; 243-246
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 2.

Tytuł:: Państwowy Instytut Geologiczny jako państwowa służba geologiczna : sto lat w służbie Niepodległej
Polish Geological Institute as the national geological survey : hundred years at the service for Poland
Autorzy:: Peryt, Tadeusz M.
Powiązania:: https://bibliotekanauki.pl/articles/2074288.pdf
Data publikacji:: 2019
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Polski Przegląd Geologiczny
prawo geologiczne i górnicze
Państwowy Instytut Geologiczny
historia geologii
Polish Geological Survey
geological and mining law
Polish Geological Institute
history of geology
Opis:: The Polish Geological Institute was established in 1919 as the national geological survey within the Ministry of Industry and Trade. The initiative of a group of parliament members to appoint the Polish Geological Institute was supported by the Polish Parliament on May 30, 1919, and the official opening of the Institute took place on May 7, 1919. Two years later the PGI status and budget were accepted by the Polish government and Józef Morozewicz has received director’s nomination from the Head of State Józef Piłsudski. In March 1938, the President of Poland accepted a new decree concerning geological survey of Poland which was composed of the Polish Geological Institute and the State Geological Council. The role of the PGI grew and the budget substantially increased, but this positive trend was stopped due to the beginning of World War II. During the first post-war years, regional and basic studies made it possible to establish a geological model of Poland leading to great discoveries of mineral deposits in the fifties. The decree of October 8, 1951 adjusted the organization forms of the geological survey to the system of central planning and the domination of state property, and the institute (with the name changed to the Geological Institute) became a scientific institution. During the first years the institute experienced good conditions of development, and a great progress in the knowledge of geology of Poland combined with the basic and regional studies that led to significant discoveries and documentation of mineral deposits. However, already in the seventies the first signs of crisis in geology became evident. In 1985, the Ministry of Environmental Protection and Mineral Resources was established, the Central Board of Geology was disbanded, and many tasks of geological survey returned to the institute, hence this turned out to be appropriate to return to the historical name, Polish Geological Institute, which took place on June 19, 1987. Since January 1, 2012, the Polish Geological Institute has served as the Polish geological survey on the basis of the Act of June 9, 2011, and earlier, since January 1, 2002, legally specified tasks of the Polish geological survey has been assigned to the PGI. On February 24, 2009 the Council of Ministers gave the PGI a status of National Research Institute, and this implied the adding this new status to the name of the Polish Geological Institute. For the century the Polish Geological Institute has successfully fulfilled all the basic responsibilities and commitments that are conventionally assigned to national geological surveys, and is a model example of modern national geological survey of very wide expertise.
Źródło:: Przegląd Geologiczny; 2019, 67, 7; 519--534
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 3.

Tytuł:: 100 lat państwowej służby geologicznej w Państwowym Instytucie Geologicznym
Hundred years of the national geological survey within the Polish Geological Institute
Autorzy:: Peryt, Tadeusz, Marek
Powiązania:: https://bibliotekanauki.pl/articles/167463.pdf
Data publikacji:: 2019
Wydawca:: Stowarzyszenie Inżynierów i Techników Górnictwa
Tematy:: państwowa służba geologiczna
prawo geologiczne i górnicze
Państwowy Instytut Geologiczny
Polish Geological Survey
geological and mining law
Polish Geological Institute
Opis:: Państwowy Instytut Geologiczny (PIG) został powołany uchwałą Sejmu Ustawodawczego w dniu 30 maja 1919 r. jako państwowa służba geologiczna w obrębie Ministerstwa Przemysłu i Handlu, a oficjalne otwarcie instytutu odbyło się 7 maja 1919 r. W marcu 1938 r. dekretem prezydenta RP powołano państwową służbę geologiczną składającą się z PIG i Państwowej Rady Geologicznej. Z kolei dekret z dnia 8.10.1951 r. przystosował formy organizacyjne służby geologicznej do systemu planowania centralnego i dominacji własności państwowej, a sam instytut (którego nazwa została zmieniona na Instytut Geologiczny) został instytutem naukowo-badawczym. W 1985 r. powołano Ministerstwo Ochrony Środowiska i Zasobów Naturalnych, a do instytutu powróciło wiele zadań służby geologicznej, z tego też względu właściwym był powrót do historycznej nazwy – PIG, co nastąpiło 19.06.1987 r. Od 1.01.2012 r. PIG pełni funkcję państwowej służby geologicznej, a wcześniej – od 1.01.2002 r. – instytutowi powierzono zadania państwowej służby geologicznej. W dniu 24.02.2009 r. Rada Ministrów nadała PIG status państwowego instytutu badawczego. Stuletnia historia PIG pokazuje, że wszystkie podstawowe zadania tradycyjnie przypisywane państwowym służbom geologicznym były wykonywane z powodzeniem, a PIG jest modelowym przykładem współczesnej państwowej służby geologicznej o bardzo szerokich kompetencjach.
The Polish Geological Institute (PGI) was established by the Polish Parliament on May 30, 1919 as the national geological survey within the Ministry of Industry and Trade, and the official opening of the Institute took place on May 7, 1919. In March 1938, the President of Poland accepted a new decree concerning geological survey of Poland which was composed of the PGI and the State Geological Council. The decree of October 8, 1951 adjusted the organization forms of the geological survey to the system of central planning and the domination of state property, and the institute (with the name changed to the Geological Institute) became a scientific institution. In 1985, the Ministry of Environmental Protection and Mineral Resources was established, and many tasks of geological survey returned to the institute, hence this turned out to be appropriate to return, on June 19, 1987, to the historical name, PGI. Since January 1, 2012, the Polish Geological Institute has served as the Polish geological survey, and earlier, since January 1, 2002, legally specified tasks of the Polish geological survey has been assigned to the PGI. On February 24, 2009 the Council of Ministers gave the PGI a status of National Research Institute. For the century the PGI has successfully fulfilled all the basic responsibilities and commitments that are conventionally assigned to national geological surveys, and is a model example of modern national geological survey of very wide expertise.
Źródło:: Przegląd Górniczy; 2019, 75, 5; 1-13
0033-216X
Pojawia się w:: Przegląd Górniczy
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 4.

Tytuł:: Rola nauki w państwowej służbie geologicznej
Science in the national geological survey
Autorzy:: Peryt, Tadeusz
Głuszyński, Andrzej
Powiązania:: https://bibliotekanauki.pl/articles/2076080.pdf
Data publikacji:: 2020
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Państwowy Instytut Geologiczny
badanie geologiczne
nauka
Polish Geological Institute
geological survey
science
Opis:: For a century - since the initiative of a group of parliament members to constitute the Polish Geological Institute (PGI) was supported by the Polish Parliament on May 30, 1919 - the PGI has success fully fulfilled all basic responsibilities and commitments that are conventionally assigned to national geological surveys. Like in the past, in modern geological surveys the research is of great importance and it is clear that they cannot exist without science, the same applies to the PGI. The scientific knowledge achieved during the implementation of geological survey tasks is important for the society and the country's development.
Źródło:: Przegląd Geologiczny; 2020, 68, 5; 312--318
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 5.

Tytuł:: The stratigraphy of Zechstein strata in the East European Craton of Poland : an overview
Autorzy:: Peryt, Tadeusz Marek
Skowroński, Leszek
Powiązania:: https://bibliotekanauki.pl/articles/2055871.pdf
Data publikacji:: 2021
Wydawca:: Polskie Towarzystwo Geologiczne
Tematy:: Zechstein
stratigraphy
palaeogeography
East European Craton
Main Dolomite
Platy Dolomite
Polska
Opis:: The sedimentary and stratigraphic patterns established for Zechstein of the western part of the Peribaltic Syneclise (and in particular the eastern Łeba Elevation) were applied to other parts of the East European Craton (EEC) in Poland: the eastern Baltic Syneclise and the Podlasie region. A very large number of mostly fully-cored borehole sections in the Puck Bay region certainly predestines the eastern Łeba Elevation area to use it as a model. The most part of the EEC, except of its part adjacent to the Teisseyre-Tornquist Zone, during the Zechstein deposition represents the marginal parts of the basin. The fauna occurring in the Zechstein carbonate deposits of the EEC makes it possible to distinguish between the Zechstein Limestone and the younger carbonate strata, but certainly not between the Main Dolomite and the Platy Dolomite and hence the facies models for the Zechstein that have been previously developed in the western part of the Peribaltic Syneclise augmented by sequence stratigraphic approach seem to be the best tool to apply in other peripheral areas in the EEC area. The Zechstein sequence in the western part of the Peribaltic Syneclise consists, in general terms, of three parts: (1) carbonate platform of the Zechstein Limestone (occurring only in the north-westernmost corner of the study area and passing into basin facies dominant in the most part of the area); (2) the PZ1 evaporite platform system composed of sulphate platforms and adjacent basin system and constituting the major part of the Zechstein sequence; and (3) the Upper Anhydrite-PZ3 cover. There is a consensus, as far as the western part of the Peribaltic Syneclise is concerned, that the Platy Dolomite platform is wider than the Main Dolomite platform. In the easternmost part of the Peribaltic Syneclise, the stratigraphical interpretations are diverse. We have included the anhydrite overlying the Zechstein Limestone into the Upper Anhydrite, and concluded that the overlying interbedded mudstone and anhydrite also belong to the Upper Anhydrite. When above the Upper Anhydrite one carbonate unit occurs, it is assigned either to the Main Dolomite and Platy Dolomite, or to the Platy Dolomite. The same conclusion is proposed for the marginal parts of the Podlasie Bay. The deposition of Zechstein Limestone resulted in the origin of carbonate platforms along the basin margins which changed an inherited topographic setting. The Lower Anhydrite deposits are lowstand systems tracts (LST) deposits, lacking in more marginal parts of the western and eastern Peribaltic Syneclise and in the major part of the Podlasie Bay. The accommodation space existed and/or created during the Lower Anhydrite and the Oldest Halite deposition in the Baltic and Podlasie bays was filled and at the onset of the Upper Anhydrite deposition, a roughly planar surface existed except in the area adjacent to the main Polish basin. The Upper Anhydrite deposits are transgressive systems tracts deposits and then highstand systems tracts deposits and they encroached the Zechstein Limestone platforms. The Upper Anhydrite deposition was terminated by sea level fall, and the Upper Anhydrite deposits in the marginal areas became subject to karstification. The Main Dolomite transgression took place in several phases but its maximum limit did not reach the Upper Anhydrite limit. The deposition of the PZ2 chlorides (LST deposits) resulted in the filling of the accommodation space that was inherited after the deposition of the Main Dolomite and the Basal Anhydrite. Subsequently, the area became exposed, and marine deposits (Grey Pelite and Platy Dolomite) related to the last major transgression during the life of the Zechstein basin that resulted in a flooding of the exposed surface of older Zechstein deposits, including the area that was emergent during deposition of the PZ2 cycle. Microbial carbonates, being stromatolites and thrombolites, are a common feature of all Zechstein carbonate units but in particular this is the case of the Platy Dolomite. There are no direct premises allowing for convincing settlement doubts regarding the stratigraphical position of the upper carbonate unit in many cases, but several lines of evidence suggest that, as in the entire Zechstein basin, the Main Dolomite considerably shifted basinward, and the Platy Dolomite – landward, although it is difficult to ascertain whether the original Platy Dolomite extent was similar to or greater than the limit of the Zechstein Limestone as elsewhere in the Zechstein Basin.
Źródło:: Annales Societatis Geologorum Poloniae; 2021, 91, 4
0208-9068
Pojawia się w:: Annales Societatis Geologorum Poloniae
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 6.

Tytuł:: Sto lat Państwowego Instytutu Geologicznego : zarys historii materialnej
One hundred years of the Polish Geological Institute : an outline of the material history
Autorzy:: Wołkowicz, Stanisław
Peryt, Tadeusz M.
Powiązania:: https://bibliotekanauki.pl/articles/2074292.pdf
Data publikacji:: 2019
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Historia Państwowego Instytutu Geologicznego
siedziba warszawska
Oddziały regionalne PIG
History of the Polish Geological Institute
Warsaw headquarters
PGI regional branches
Opis:: Established a few months after regaining independence in 1918, the Polish Geological Institute was carrying out research aimed at ensuring the supply of necessary mineral raw resources to the domestic industry. The director of the Institute, Prof. J. Morozewicz as well as the state authorities were aware of the fact that for the proper functioning of the Institute suitable headquarter was needed. Therefore, already in the mid-1919, the appropriate area and financial resources were allocated for the construction of large buildings, the designer of which S W0łk0wicZ T M Pervt was Prof. M. Lalewicz. The laboratory pavilion was opened in 1926. The main building, which was put into use in 1936 and rebuilt after the destruction during World War II, has been the pride of the Institute until today. The extension of the state and a wide range of research issues meant that already in 1921, it was necessary to establish the Upper Silesian Station in Dąbrowa Górnicza, whose activity was focused on the coal geology. The Geological Station in Borysław, operating in the structure of the PGI since 1920, was transformed three years later into the Oil and Salt Department of the PGI, which closely co-operated with the Carpathian oil industry. The Holy Cross Mountain research group was located during 1937-1955 in the family home of Jan Czarnocki. After World War II, due to the significant intensification of geological research and exploration in Poland, new regional divisions of the Institute were established that currently have their headquarters in Kraków, Sosnowiec, Wrocław, Kielce, Gdańsk and Szczecin; all have the rank of branches. The organizational structure of the PGI is of an extremely regional nature, and the research issues of individual branches are mostly related to the recognition of the geological structure and mineral resources occurring in a given region. In addition, the Polish Geological Institute possesses 8 core repositories.
Źródło:: Przegląd Geologiczny; 2019, 67, 7; 507--518
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 7.

Tytuł:: The stratigraphy of Zechstein strata in the East European Craton of Poland : an overview
Autorzy:: Peryt, Tadeusz Marek
Skowroński, Leszek
Powiązania:: https://bibliotekanauki.pl/articles/2060632.pdf
Data publikacji:: 2021
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Zechstein
stratigraphy
palaeogeography
East European Craton
Main Dolomite
Platy Dolomite
Polska
Opis:: The sedimentary and stratigraphic patterns established for Zechstein of the western part of the Peribaltic Syneclise (and in particular the eastern Łeba Elevation) were applied to other parts of the East European Craton (EEC) in Poland: the eastern Peribaltic Syneclise and the Podlasie region. A very large number of mostly fully-cored borehole sections in the Puck Bay region certainly predestines the eastern Łeba Elevation area to use it as a model. The most part of the EEC, except of its part adjacent to the Teisseyre-Tornquist Zone, during the Zechstein deposition represents the marginal parts of the basin. The fauna occurring in the Zechstein carbonate deposits of the EEC makes it possible to distinguish between the Zechstein Limestone and the younger carbonate strata, but certainly not between the Main Dolomite and the Platy Dolomite and hence the facies models for the Zechstein that have been previously developed in the western part of the Peribaltic Syneclise augmented by sequence stratigraphic approach seem to be the best tool to apply in other peripheral areas in the EEC area. The Zechstein sequence in the western part of the Peribaltic Syneclise consists, in general terms, of three parts: (1) carbonate platform of the Zechstein Limestone (occurring only in the north-westernmost corner of the study area and passing into basin facies dominant in the most part of the area); (2) the PZ1 evaporite platform system composed of sulphate platforms and adjacent basin system and constituting the major part of the Zechstein sequence; and (3) the Upper Anhydrite-PZ3 cover. There is a consensus, as far as the western part of the Peribaltic Syneclise is concerned, that the Platy Dolomite platform is wider than the Main Dolomite platform. In the easternmost part of the Peribaltic Syneclise, the stratigraphical interpretations are diverse. We have included the anhydrite overlying the Zechstein Limestone into the Upper Anhydrite, and concluded that the overlying interbedded mudstone and anhydrite also belong to the Upper Anhydrite. When above the Upper Anhydrite one carbonate unit occurs, it is assigned either to the Main Dolomite and Platy Dolomite, or to the Platy Dolomite. The same conclusion is proposed for the marginal parts of the Podlasie Bay. The deposition of Zechstein Limestone resulted in the origin of carbonate platforms along the basin margins which changed an inherited topographic setting. The Lower Anhydrite deposits are lowstand systems tracts (LST) deposits, lacking in more marginal parts of the western and eastern Peribaltic Syneclise and in the major part of the Podlasie Bay. The accommodation space existed and/or created during the Lower Anhydrite and the Oldest Halite deposition in the Baltic and Podlasie bays was filled and at the onset of the Upper Anhydrite deposition, a roughly planar surface existed except in the area ad jacent to the main Polish basin. The Upper Anhydrite deposits are transgressive systems tracts deposits and then highstand systems tracts deposits and they encroached the Zechstein Limestone platforms. The Upper Anhydrite deposition was terminated by sea level fall, and the Upper Anhydrite deposits in the marginal areas became subject to karstification. The Main Dolomite transgression took place in several phases but its maximum limit did not reach the Upper Anhydrite limit. The deposition of the PZ2 chlorides (LST deposits) resulted in the filling of the accommodation space that was inherited after the deposition of the Main Dolomite and the Basal Anhydrite. Subsequently, the area became exposed, and marine deposits (Grey Pelite and Platy Dolomite) related to the last major transgression during the life of the Zechstein basin that resulted in a flooding of the exposed surface of older Zechstein deposits, including the area that was emergent during deposition of the PZ2 cycle. Microbial carbonates, being stromatolites and thrombolites, are a common feature of all Zechstein carbonate units but in particular this is the case of the Platy Dolomite. There are no direct premises allowing for convincing settlement doubts regarding the stratigraphical position of the upper carbonate unit in many cases, but several lines of evidence suggest that, as in the entire Zechstein basin, the Main Dolomite considerably shifted basinward, and the Platy Dolomite - landward, although it is difficult to ascertain whether the original Platy Dolomite extent was similar to or greater than the limit of the Zechstein Limestone as elsewhere in the Zechstein Basin.
Źródło:: Geological Quarterly; 2021, 65, 4; 21--27
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 8.

Tytuł:: Badania złóż soli kamiennej i potasowo-magnezowej prowadzone w Państwowym Instytucie Geologicznym
PGI research of rock salt and K-Mg deposits
Autorzy:: Czapowski, Grzegorz
Peryt, Tadeusz, Marek
Powiązania:: https://bibliotekanauki.pl/articles/2074293.pdf
Data publikacji:: 2019
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: sole
złoża
baden
cechsztyn
sedymentologia
geochemia
salts
deposits
Baden
Zechstein
sedimentology
geochemistry
Opis:: Middle Miocene Badenian salt, occurring in the frontal zone of the Carpathian Overthrust (southern Poland), and the Upper Permian (Zechstein) bedded and diapir salt deposits, have been the subject of the research by PGI scientists. Many salt deposits were discovered by the PGI, but in particular, the greatest achievement related to the origin of salt deposits is the reconstruction of sedimentary environments and conditions based on detailed sedimentological and geochemical analyses.
Źródło:: Przegląd Geologiczny; 2019, 67, 7; 594--598
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 9.

Tytuł:: Wydawnictwa Państwowego Instytutu Geologicznego 1919–2019
Publishing activities of the Polish Geological Institute during 1919–2019
Autorzy:: Dąbrowska-Jędrusik, Ewa
Peryt, Tadeusz Marek
Powiązania:: https://bibliotekanauki.pl/articles/2074290.pdf
Data publikacji:: 2019
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: publikacje
czasopisma naukowe
mapy
atlas
Państwowy Instytut Geologiczny
publications
scientific journals
maps
atlases
Polish Geological Institute
Opis:: Publication activities have played an important role in the life of the Polish Geological Institute (PGI) since its foundation in 1919. In 1919 the first geological map and in 1920 the first text publication were put out whereas in 1921 the first series appeared that has been issued till today: Transactions of the PGI (Prace Państwowego Instytutu Geologicznego). In 1938, the series Bulletin of the PGI (Biuletyn Państwowego Instytutu Geologicznego), and in 1957 the Geological Quarterly, the flag journal of the PGI, were initiated. Their first mission was to disseminate results of studies conducted by the PGI scientists, but since 1999 the Geological Quarterly has been a truly international journal. The PGI co-edits two other international journals (Geologica Carpathica, Volumina Jurasica) and since 1992 has been a publisher of the most popular Polish geological journal, Przegląd Geologiczny. This journal was established in 1953, but the first publisher was Wydawnictwa Geologiczne that stem from the PGI in 1953, and finally in 2000 all publication activities returned to the PGI. In addition, a range of various books has been published, including a monumental scientific synthesis entitled Geology of Poland that was initiated in 1963; its first part was published in 1968 and the last one in 2004 (altogether 25 parts in six volumes). After World War II, one of the top priorities of the PGI was to elaborate various synthetic, detailed and special maps as well as atlases, and this activity, which otherwise is the proof of the notable increase of our knowledge on the geology of Poland, belongs to the great achievements of the PGI. Within a century, about 15,000 geological maps were published. Since the last decade, a number of publications dealing with various tasks of the Polish geological survey and the Polish hydrogeological survey has distinctly been increased
Źródło:: Przegląd Geologiczny; 2019, 67, 7; 610--616
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 10.

Tytuł:: Foraminiferal and calcareous nannoplankton biostratigraphy of the upper Badenian–lower Sarmatian strata in the SE Polish Carpathian Foredeep
Autorzy:: Peryt, Danuta
Garecka, Małgorzata
Peryt, Tadeusz Marek
Powiązania:: https://bibliotekanauki.pl/articles/2058716.pdf
Data publikacji:: 2021
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Middle Miocene
Carpathian Foredeep Basin
foraminifera
nannofossils
palaeoenvironments
Opis:: The Badenian/Sarmatian boundary in the Central Paratethys has been traditionally identified by the faunal turnover recording an important environmental change possibly controlled by the change from marine to brackish conditions. The strata below the Badenian/Sarmatian boundary in the northern Carpathian Foredeep are included into the Pecten beds, and those above it into the Syndesmya beds. Foraminiferal study of the Babczyn 2 borehole which is one of the crucial sections in the northern Carpathian Foredeep, well-known for the depositional age of rhyolite tuff within the Pecten beds dated by Śliwiński et al. (2012) at 13.06 ±0.11 Ma, indicated that in fact the boundary occurs within the Syndesmya beds. This conclusion is based upon the rapid change from a stenohaline foraminiferal fauna to a euryhaline one, and the appearance of the species Anomalinoides dividens, the taxon regarded as the marker for the Sarmatian. In the Babczyn 2 and Cieszanów 1 (located ~2.5 km basinward of Babczyn 2) boreholes, Anomalinoides dividens appears 3.1–3.8 m above the replacement of stenohaline by euryhaline foraminifers. The calcareous nannoplankton study shows that the upper Badenian and the lower Sarmatian strata in the studied sections represent the NN6, undivided NN6-NN7, and NN7 zones.
Źródło:: Geological Quarterly; 2021, 65, 1; 18
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

Artykuł

Zmień widok

na półce

Skocz do pozycji: 11.

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

Zmień widok

na półce

Skocz do pozycji: 12.

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

Zmień widok

na półce

Informacja

Wyszukujesz frazę "Peryt, Tadeusz" wg kryterium: Autor

Źródło danych

Dostawca treści

Kolekcja

Rok wydania

Wydawca

Temat

Autor

Typ dokumentu

Język