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Erinnerungsort Lublin – literarische Narrationen über die Stadt und ihre jüdischen Bewohner bei Alfred Döblin und Hanna Krall

Anna Pastuszka

Kwartalnik Neofilologiczny | 2019 | No 1 | 60-71 | DOI: 10.24425/kn.2019.126504

Keywords place of memory Lublin Alfred Döblin Hanna Krall Jews of Lublin

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Abstract

The article presents Lublin through the analysis of two literary texts that show the existence of the Jewish population of the city and the destruction and absence of Jews from Lublin. Döblin describes in his travelogue Journey to Poland (1925) the parallel existence of the Jewish and Polish city of Lublin in the 1920’s. Krall documents in her literary reportage Exceptionally long line the extermination of the Jewish community and the suppression of the memory of it in Polish collective memory.

Authors and Affiliations

Anna Pastuszka

The Find of False Groschen of King Sigismund III Vasa (1587–1632) from Lublin

Miłosz Huber Tomasz Markiewicz

Wiadomości Numizmatyczne | 2020 | Rok LXIV | 245-264 | DOI: 10.24425/wn.2020.136913

Keywords counterfeiting of coins groschen Sigismund III Vasa Lublin

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Abstract

The assemblage of coins found in the Old Town district of Lublin (6a, Wincentego Pola St., presently known as Archidiakońska St.) on 1 July 1981 consists of 21 false groschen of Sigismund III Vasa (1587–1632) and 2 fragments of unspecified coins. As a result of the research analysis, it has been found that the coins were minted in tin-coated copper. Despite the fact that the dates are decipherable only on 10 groschen coins, it may be inferred from the identity of the coin dies that 15 of them (71.4%) bear the year 1608, while 5 (23.8%) – 1607. No date has been determined for only one coin. The groschen of 1607, struck with the use of one pair of coin dies, imitate the bust / eagle type. This particular variation tends to prevail also among the pieces with the date 1608 (13 out of a total number of 15 pieces), which had been coined with the use of two pairs of dies. 1 groschen with a bust and 2 groschen with a crown image had been struck by means of some other coin dies. The fact that the forged coins were found at the site of the former townhouse owned by the mayor Jan Szembek (since 1608) allows us to presume that they may have been deposited there as a result of some administrative action taken against the illegal practice. Beginning from the early decades of the 17th century, conditions for the growth of such practices had been created and fuelled by the atmosphere of the increasing economic crisis and the resulting perturbations spreading across the monetary markets of the Polish-Lithuanian Commonwealth.

Authors and Affiliations

Miłosz Huber

1

e-mail:

ORCID:

Tomasz Markiewicz

2

e-mail:

ORCID:

Katedra Geologii, Gleboznawstwa i Geoinformacji UMCS, Al. Kraśnickie 2cd 20-718 Lublin
Muzeum Narodowe w Lublinie, ul. Zamkowa 9, 20–117 Lublin

Historyczne i artystyczne wartości fotografii: lubelskie zdjęcia Stefana Kiełszni

Marta Kubiszyn

Historyka Studia Metodologiczne | 2019 | tom 49 | 173-199 | DOI: 10.24425/hsm.2019.130580

Keywords Stefan Kiełsznia Lublin photography Jewish district

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Abstract

The article discusses Stefan Kiełsznia’s collection within the theoretical framework of Gillian Rose’s concept concerning analysis of visual materials. Questions regarding the composition and contents of the photographs as well as the historical and social circumstances of their origin, together with the place of the series within Stefan Kiełsznia’s oeuvre, are juxtaposed with issues regarding perception of these images as documents of the non-existent Jewish quarter.

Authors and Affiliations

Marta Kubiszyn

Garden as a meeting place for a child with nature – a project to develop the playground at Radomska street in Lublin

Margot Dutkiewicz Monika Kowalczyk Patryk Krupiński

Teka Komisji Urbanistyki i Architektury Oddziału Polskiej Akademii Nauk w Krakowie | 2018 | 293–302

Keywords child Lublin natural playground green areas

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Abstract

Celem pracy było przedstawienie relacji natura-ogród-dziecko na przykładzie projektu zagospodarowania skweru znajdującego się w dzielnicy Węglin Południowy w Lublinie. Współcześnie większość terenów rekreacyjnych dla dzieci wyposażanych jest w urządzenia umożliwiające dzieciom standardowe zabawy ruchowe tj. huśtanie się, kręcenie w kółko, wspinanie. W niestandardowym podejściu do tematu – tereny zieleni miejskiej mogą należeć do nielicznych miejsc, gdzie wśród otoczenia roślin i zwierząt, dzieci mogą rozwijać swoją kreatywność, pasje, utożsamiać się z daną przestrzenią oraz nabywać nowych doświadczeń. W przedstawionej pracy ukazano również konieczność zwiększenia liczby miejsc wypoczynku dla osób w różnych przedziałach wiekowych.

Authors and Affiliations

Margot Dutkiewicz

Monika Kowalczyk

Patryk Krupiński

“My Theatre I see immense”. Visions and (would-be) Realisation of the Dramatic Theatre in Lublin as an Exemplum of Modern Theatre Architecture

Piotr Majewski

Rocznik Historii Sztuki | 2023 | No XLVIII | 98-118 | DOI: 10.24425/rhs.2023.147050

Keywords theatre architecture architecture of Central and Eastern Europe modernism art in the period of the People’s Republic of Poland Juliusz Osterwa Theatre in Lublin competition for the construction of the DramaticTheatre in Lublin Centre for the Meeting of Cultures in Lublin

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Abstract

The article presents the history of the competition and design of the building originally intended for the Juliusz Osterwa Theatre in Lublin (currently the Centre for the Meeting of Cultures). Both the concepts of the location of the building and urban conditions were discussed, as well as various conceptual designs of the theatre, awarded and distinguished in an architectural competition at the turn of the 1950s and 1960s. In the further part of the article, the concept of the experimental scene, proposed by Kazimierz Braun in the early 1970s, is discussed. The background for the reconstruction of the history of the design and construction of the building are changes in the style and arrangement of the modern theatre architecture, with particular emphasis on Central and Eastern Europe.

Authors and Affiliations

Piotr Majewski

1

Uniwersytet Marii Curie-Skłodowskiej w Lublinie

Modernization on credit: The Szopki sketch comedy show in interwar Lublin

Aleksander Wójtowicz

Ruch Literacki | 2021 | No 4 (367) | 553-570 | DOI: 10.24425/rl.2021.138745

Keywords Sketch comedy in Poland in the interwar period satire popular culture poetic avant-garde Lublin Jan Arnsztajn (1897–1934)

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Abstract

The sketch comedy Szopki, a show staged irregularly (1927–1931) by a trio of poets who clustered round the avant-garde magazine Reflektor was a fascinating artistic project combining literary aspiration and popular culture. This article tries to position Szopki in the context of the burgeoning entertainment industry and the specific social, political and economic conditions of Lublin, a provincial centre that joined an ambitious modernization project. However, to continue the Great Lublin Project the town needed to borrow more money it could not possibly pay back. No wonder the official narrative of modernization came under an unending barrage of ridicule and derision while local satire revelled in words like crisis, credit, bankruptcy, seizure and sale.

Bibliography

● J. Arnsztajn, K. Bielski, W. Gralewski, Pierwsza Szopka Reflektora, w zbiorach Muzeum Józefa Czechowicza w Lublinie, sygn. MC 143 R.
● J. Arnsztajn, K. Bielski, Druga Szopka Reflektora, w Zbiorach Specjalne Wojewódzkiej Biblioteki Publicznej im. H. Łopacińskiego w Lublinie, sygn. 2156.
● Z. Bauman, Płynna nowoczesność, przeł. T. Kunz, Kraków 2006.
● M. Berman, „Wszystko, co stałe, rozpływa się w powietrzu”. Rzecz o doświadczeniu nowoczesności, przeł. M. Szuter, Kraków 2006.
● K. Bielski, Most nad czasem, Lublin 1963.
● Ł. Biskupski, Miasto atrakcji. Narodziny kultury masowej na przełomie XIX i XX wieku. Kino w systemie rozrywkowym Łodzi, Warszawa 2013.
● T. Bocheński, Szopka lubelska, „Ziemia Lubelska” 15.05.07.
● J. Cymerman, D. Gac, G. Kondrasiuk, Scena Lublin, Lublin 2017.
● J. Cymerman, A. Wójtowicz, Uwagi wydawców, [w:] Józef Czechowicz, Pisma zebrane, t. 9, Varia, oprac. Jarosław Cymerman, Aleksander Wójtowicz, Lublin 2013, s. 653–654.
● J. Czechowicz, Pisma zebrane, t. 1, Wiersze i poematy, opr. J.F. Fert, Lublin 2012.
● A. Czuchryta, Przemysł rolno-spożywczy w województwie lubelskim w latach 1918–1939, Lublin 2008.
● D. Fox, Kabarety i rewie międzywojennej Warszawy. Z prasowego archiwum dwudziesto-lecia, Katowice 2007.
● H. Gawarecki, O dawnym Lublinie, Lublin 1974.
● Historia Lublina w liczbach, A. Jakubowski, U. Bronisz, E. Łoś, Lublin 2017.
● M. Hemar, J. Lechoń, A. Słonimski, J. Tuwim, Szopki Pikadora i Cyrulika Warszawskiego, opr. T. Januszewski, Warszawa 2013.
● E. Jabłońska-Depuła, Wielkomiejski plan rozwoju Lublina z 1924 roku, [w:] Lublin w dziejach i kulturze Polski, pod red. T. Radzika i A. Witusika, Lublin 1997.
● T. Kłak, Czasopisma awangardy, cz. 1, 1919–1931, „Polska Akademia Nauk”, Wrocław 1978.
● E. Krasiński, Warszawskie sceny 1918–1939, Warszawa 1976.
● S. Kruk, Teatr Miejski w Lublinie 1918–1939, Lublin 1997.
● Kuligowska-Korzeniewska, Kabaret w złym mieście podczas Wielkiej Wojny oraz M. Szydłowska, Gwiazdy i meteory lwowskiego „Ula”, [w:] Kabaret – poważna sprawa, pod red. D. Fox i J. Mikołajczyka, Katowice 2015.
● Z. Landau, Pożyczki ulenowskie, „Najnowsze Dzieje Polski: Materiały i Studia z Okresu 1914–1939” 1958, t. 1.

Authors and Affiliations

Aleksander Wójtowicz

1

e-mail:

ORCID:

Instytut Filologii Polskiej, Uniwersytet Marii Curie-Skłodowskiej

Zabytkowe ogrody klasztorne we współczesnym Lublinie

Anna Mirosław Krystyna Pudelska

Teka Komisji Architektury, Urbanistyki i Studiów Krajobrazowych | 2011 | No VII

Keywords klasztory ogrody przyklasztorne przekształcenia Lublin

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Abstract

Założenia klasztorne na terenie Lublina mają bogatą historię. Pierwszy powstał już w XIV w. Z czasem do miasta sprowadzano kolejne zakony, dla których fundowano nowe miejsca pod zabudowę. Założenia lokowane poza murami miasta były otoczone pokaźnymi ogrodami. Do dóbr zakonnych należały także pola, łąki, folwarki, a nawet wsie. Przez szereg lat zakonnicy powiększali swoje włości, zabezpieczając w ten sposób finansowanie działalności, którą prowadzili. Po okresie świetności przychodzą ciężkie czasy konfliktów zbrojnych obejmujących Lublin. W tym okresie założenia klasztorne ulegają licznym zniszczeniom, część przekształcana jest na cele świeckie, a przylegające do nich ogrody są dzielone na mniejsze parcele, przeznaczane pod zabudowę lub są sprzedawane. Z istniejących w XVIII w. 18 klasztorów do czasów współczesnych przetrwało 14. Wszystkie są wpisane do Rejestru Zabytków Województwa Lubelskiego, a tylko 6 z nich stanowi do dzisiaj własność zakonów. Ogrody przy zachowanych obiektach różnią się powierzchnią i funkcją od tych z okresu swojej świetności. Ich obszar w obrębie miasta od XVIII w. do czasów współczesnych zmniejszyła się o ponad połowę. Cztery z nich uległy nie-wielkim przekształceniom, a w niezmienionej formie pozostały tylko wirydarze w 9 dawnych klasztorach. Pozostała zieleń pełni funkcje ogrodów przyszpitalnych, przykościelnych lub skwerów miejskich.

Authors and Affiliations

Anna Mirosław

Krystyna Pudelska

Dzielnica Czechów w Lublinie - geneza układu urbanistycznego

Natalia Przesmycka

Teka Komisji Architektury, Urbanistyki i Studiów Krajobrazowych | 2015 | No 3

Keywords Lublin Czechów konkursy urbanistyczne projektowanie urbanistyczne

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Abstract

Geneza planowania i projektowania urbanistycznego układu Czechowa sięga okresu międzywojennego. Na dzisiejszy układ urbanistyczny składają się nie tylko opracowania dla poszczególnych osiedli powstające od początku lat 70. XX wieku, ale również przybliżony w artykule, wcześniejszy dorobek planistyczny i projektowy.

Authors and Affiliations

Natalia Przesmycka

Quality of coal from exploited seams in LW “Bogdanka” S.A. (Lublin Coal Basin). = Jakość węgla eksploatowanych pokładów w LW „Bogdanka” S.A. (Lubelskie Zagłębie Węglowe)

Jacek Misiak

Gospodarka Surowcami Mineralnymi - Mineral Resources Management | 2012 | vol. 28 | No 4 | 137-149 | DOI: 10.2478/v10269-012-0034-y

Keywords Lublin Coal Basin Carboniferous coal quality

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Abstract

The quality of coal has been analyzed basing on the data from geological exploration and chemical – geological analyses of coal carried out on the samples obtained from the boreholes and mining pits. The operated coal seams indexed as 382 and 385/2 reveals the changeable morphology due to the thickness of carbon shoals and stent intergrowths. The other parameters, such as the ash content or the calorific value are strongly linked with the non-coal rock interlayers, which presence causes the decrease in the calorific value and increase in the amount of after-burning ash. These parameters are less dependable on the sedimentation environment of the coal formation material. The content of total sulfur in the analyzed seams does not show any link with the values of the parameters analyzed before. The total sulfur is made up from sulphide gathered in coal and sulphates deriving from the decomposition of plants and supplied by deposit waters in different phases of coal seam formation. The obtained results could be useful in the reconnaissance of the prospective seams lying below the currently exploited ones (e.g. 389) and the seams in the neighboring areas.

Authors and Affiliations

Jacek Misiak

e-mail:

ORCID:

Problems of the design of the landscape of small towns. The case of Frampol

Małgorzata Sosnowska

Teka Komisji Architektury, Urbanistyki i Studiów Krajobrazowych | 2015 | No 1

Keywords small towns Lublin region Frampol urban landscape design

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Abstract

The Lublin region has a rich history of coexistence and interpenetration of different traditions, cultures and religions, witnessed by its cities and towns. Small towns of the Lublin region are now facing a variety of spatial problems which are related to, among others, the organization and revitalization of public spaces, progressive scattering of housing development or changes in the organisation of traffic. The aim of this article is to present problems connected with landscape design and the revitalization of small towns of the Lublin region as exemplified by Frampol.

Authors and Affiliations

Małgorzata Sosnowska

Zapomniany dwór Gorajskich przy ul. Bernardyńskiej 12 w Lublinie

Krzysztof Janus

Teka Komisji Architektury, Urbanistyki i Studiów Krajobrazowych | 2015 | No 1

Keywords dwór Gorajskich badania architektoniczne wąwóz przy ul. Bernardyńskiej ul. Bernardyńska (Lublin)

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Abstract

W pracy opisano skomplikowaną i bujną historię budynku dawnego dworu Gorajskich przy ul. Bernardyńskiej 12 w Lublinie. Uwzględniono powszechnie znane fakty i dokumenty historyczne z życia budynku jak i te dopiero poznane. Przy uwzględnieniu istniejących prac badawczych i projektów oraz oględzin i badań własnych udało się wykonać analizę architektoniczną, z wykonaniem rozwarstwienia i określenia faz przekształceń budynku. Praca ta pozwoliła na umieszczenie dworu Gorajskich jako jednego z zapomnianych ale ciągle zachowanych dworów magnackich powstałych w XVII wieku na lubelskim Żmigrodzie.

Authors and Affiliations

Krzysztof Janus

Hydrological characteristics of the Krężniczanka River

Zdzisław Michalczyk Stanisław Chmiel Sławomir Głowacki Joanna Sposób Beata Zielińska

Teka Komisji Ochrony I Kształtowania Środowiska Przyrodniczego | 2017 | Vol XIV

Keywords groundwaters runoff water balance the Krężniczanka River Lublin Upland

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Abstract

The paper discusses the water resources of the Krężniczanka River catchment. The catchment with an area of 224.9 km2 is located south-west of Lublin. The characteristics of the groundwaters and runoff were determined based on hydrological and hydrogeological materials of the Department of Hydrology of the Maria Curie-Skłodowska University (UMCS). Mean runoff in the period from 2010 to 2016 amounted to 125.7 mm, precipitation 629.4 mm, and evapotranspi-ration 503.7 mm. A strong relationship was determined between the rhythm of runoff and ground-water level fluctuations. The contribution of groundwater supply in total runoff equalled 81.5%.

Authors and Affiliations

Zdzisław Michalczyk

Stanisław Chmiel

Sławomir Głowacki

Joanna Sposób

Beata Zielińska

The role of mineral matter in the concentration of phosphorus in bituminous coal seams from the Lublin Formation in the Lublin Coal Basin in Poland

Henryk Ryszard Parzentny

Gospodarka Surowcami Mineralnymi - Mineral Resources Management | 2018 | vol. 34 | No 3 | 53-70 | DOI: 10.24425/122582

Keywords phosphorus bituminous coal coal seams Lublin Coal Basin

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Abstract

The study included bituminous coal seams (30 samples coal from the Bogdanka and Chełm deposits)

of the Lublin Formation, the most coal-bearing strata in the best developed and recognized in

terms of mining parts of the Lublin Coal Basin in Poland. High phosphorus concentrations in coal of

the Lublin Formation were found (1375 g/Mg) as well as P2O5 in coal ash (2.267 wt%). The phosphorus

contents in coal and coal ash from the 385 and 391 coal seams in the area of the Lubelski Coal Bogdanka

Mine and in the area of its SE neighbor is the highest (max. 2.644 wt. % in coal and 6.055 wt. %

of P2O5 in coal ash). It has been shown that mineral matter effectively affects phosphorus contents

in coal and coal ash. At the same time, phosphate minerals (probably apatite and crandallite) present

in kaolinite aggregates of tonsteins contain the most of phosphorus and have the greatest impact on

the average P content in the 382, 385, 387, and 391. The secondary source of phosphorus in these

coal seams and main source of phosphorus in these coal deposits that do not contain mineral matter

of pyroclastic origin (378, 389, 394) may be clay minerals, which absorbed phosphorus compounds

derived from organic matter released during coalification. Phosphorus-rich ash from the combustion

of the Lublin Formation coal tend to be environmentally beneficial to the environment and also useful

for improving the soil quality. Due to the low degree of coalification and high content of phosphorus

in coal, this coals of little use for coking.

Authors and Affiliations

Henryk Ryszard Parzentny

Analysis of the Objectives and the Level of Implementation of the Spatial Development Plan of the Central Coal Region – the Lublin Coal Basin (CRW-LZW)

Michał Tomasz Dmitruk

Archives of Mining Sciences | 2021 | vol. 66 | No 4 | 543-560 | DOI: 10.24425/ams.2021.139596

Keywords mining transformation spatial planning urban planning Lublin region

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Abstract

One of the ways to reduce greenhouse gas emissions to the atmosphere is to minimise the production of fossil fuels energy, which, among others, can be achieved through gradual closure of hard and brown coal mines. However, such transformation comes with economic and social problems as well as structural changes. This article is a case study based on the objectives of the Spatial Development Plan for the Central Coal Region (CRW) – Lublin Coal Basin (LZW), developed as a consequence of the discovery of significant hard coal deposits in the north-eastern part of the Lublin voivodeship in the 1960’s. In retrospect, it can be observed that the overly ambitious objectives of the CRW-LZW urban plan were implemented only to a limited extent.
This article aims to compare the original urban planning objectives with the current development of the industrial district and to indicate the cause for such a significant limitation of the realisation of the originally planned investment. Also, the article endeavours to simultaneously emphasize which factors should be specially considered, when planning such large-scope investments, that also broadly influence demographic and urban structure of the region and the way it is functioning.
The analysis was carried out in the context of economic difficulties and the political crisis at the turn of the 1970s and 1980s, the changes in the country’s political and economic system, as well as the principles of the socio-economic concept of sustainable development implemented at the end of the 20th century, and the currently prevailing circular economy. The characteristics and analysis of the adopted design solutions were carried out, the assessment of the extent to which the planned investment was completed and what factors influenced its current condition. The collected data is summarized and compared in a table. The conclusions may prove helpful in establishing the direction of Lublin Coal Basin the development in the coming years. The described solutions and experiences may constitute the theoretical basis for accurate forecasting of the scope of similar investments in the future.

Bibliography

[1] A . Frejowski, J. Bondaruk, A. Duda, Wyzwania i szanse dla terenów po wyeksploatowanych kopalniach węgla: od czarnej do zielonej energii. Energies 14, 1385 (2021). DOI : https://doi.org/10.3390/en14051385
[2] H . Gerbelová, A. Spisto, S. Giaccaria, Regional Energy Transition: An Analytical Approach to the Slovakian Coal Regio. Energies 14, 110 (2021). DOI : https://doi.org/10.3390/en14010110
[3] L. Kolanowski, Rozwój przestrzenny Łęcznej, jako ośrodka Lubelskiego Zagłębia Węglowego. Annales Universitatis Mariae Curie-Skłodowska, Lublin 73, Sectio B (2018). DOI : https://doi.org/10.17951/b.2018.73.0.29-47
[4] L. Lehotský, M. Černík, Brown coal mining in the Czech Republic – lessons on the coal phase-out. International Issues & Slovak Foreign Policy Affairs 28, (3/4) (2019). https://www.jstor.org/stable/26905905, accessed 25.02.2021
[5] P. Oei, H. Brauers, P. Herpich, Lessons from Germany’s hard coal mining phase-out: policies and transition from 1950 to 2018. Climate Policy 20 (8), 963-979 (2020). DOI : https://doi.org/10.1080/14693062.2019.1688636
[6] E . Pietrzyk-Sokulska, R. Uberman, J. Kulczycka, The impact of mining on the environment in Poland – myths and reality. Mineral Resources Management 31 (1) (2015). DOI : https://doi.org/10.1515/gospo-2015-0009
[7] E . Sermet, J. Górecki, Podstawowe kryteria możliwości podziemnego zgazowania węgla w Lubelskim Zagłębiu Węglowym. Zeszyty Naukowe Instytutu Gospodarki Surowcami Mineralnymi i Energii Polskiej Akademii Nauk nr 83/2012, (2012). ISSN 2080-0819.
[8] A . Tajduś, A. Tokarski, Risks related to energy policy of Poland until 2040 (EPP 2040). Archives of Mining Sciences 65 (4), 877-899 (2020). DOI : https://doi.org/10.24425/ams.2020.135183
[9] K . Van de Loo, Social engineering for coal mine closures – a world bank report, the international research deficit and reflections from a German perspective. Mining Report 155 (4) (2019).
[10] B. Brylak-Szymczak, A. Link, M. Żurkowska, M. Osmulska, E. Mazurek, R. Dylewski, Łęczna. Nowe polskie miasto. Przyszłość, perspektywy. Rada Miejska w Łęcznej, Łęczna (1994).
[11] A . Frużyński, Zarys dziejów górnictwa węgla kamiennego w Polsce. Muzeum Górnictwa Węglowego, Zabrze (2012). ISBN 978-83-935614-4-5
[12] J. Kicki, B. Kozek, J. Jarosz, A. Dyczko (Ed.), 30 lat górnictwa węglowego na Lubelszczyźnie 1975-2005, Lubelski Węgiel „Bogdanka” Spółka Akcyjna, (2006). ISBN: 978-83-917727-3-X
[13] A . Zdanowski, Atlas Geologiczny Lubelskiego Zagłębia Węglowego, Państwowy Instytut Geologiczny, Warszawa, (1999). OCLC: 45743965
[14] A . Harat, Z. Adamczyk, A. Klupa, Economic and environmental aspects of the liquidation of coal mines, Proceeding of Conference: 17th International Multidisciplinary Scientific Geo Conference SGE M 2017, 29 June – 5 July, (2017). DOI : https://doi.org/10.5593/sgem2017/54/S23.035, ISSN 1314-2704
[15] J. Kaliński, Z. Landau, Gospodarka Polski w XX wieku. Wyd. 2 zmienione. Polskie Wydawnictwo Ekonomiczne, Warszawa, (2003). ISBN: 978-83-208-1428-6
[16] A Green New Deal. Joined-up policies to solve the triple crunch of the credit crisis, climate change and high oil prices, New Economics Foundation, Londyn, (2008). https://neweconomics.org/2008/07/green-new-deal, accessed: 23.11.2021
[17] EU coal regions: opportunities and challenges ahead. https://ec.europa.eu/jrc/en/news/eu-coal-regions-opportunitiesand-challenges-ahead, accessed 25.07.2021
[18] Kluczowe elementy Strategii rozwoju LW Bogdanka S.A. Obszar Wydobycie Grupy ENEA do 2030 roku (perspektywa do 2040 roku). https://ri.lw.com.pl/o-firmie-strategia, accessed 25.07.2021
[19] https://www.lw.com.pl/pl,2,aktualnosci,d264,kontynuacja_i_transformacja__nowa_strategia_lw_bogdanka_ do_2030_r.html, accessed 25.07.2021
[20] https://leczna.pl/leczna/leczna-w-liczbach, accessed 25.07.2021
[21] Letter from the President of the Management Board of Lubelski Węgiel Bogdanka, No. 227.PR.076.28.14.2021.1388.
[22] Letter of the Undersecretary of State No. UAN .1-LZW-20/79 of March 16, 1979.
[23] Directive (EU ) 2018/2001 of the European Parliament and of the Council of December 11, 2018, on the promotion of the use of energy from renewable sources, (2018).
[24] P. Czyżak, M. Hetmański, 2030 – Analiza dot. Granicznego roku odejścia od węgla w energetyce w Europie i Polsce. Instrat Policy Paper 01/2020, (2020). ISBN: 978-83-946738-3-3
[25] C . Kemfert, M. Fischedick, K. Bausch, Phasing out coal in the German energy sector interdependencies, challenges and potential solutions. German Institute for Economic Research (DIW Berlin), (2019). https://www.ecologic.eu/sites/default/files/publication/2019/3537-kohlereader_englisch-final.pdf, accessed 23.11.2021
[26] J. Porzycki, Lubelskie Zagłębie Węglowe. [In:] Przewodnik 42 Zjazdu Polskiego Towarzystwa Geologicznego Lublin, Wydawnictwo Geologiczne, (1970).
[27] J. Stochlak, K. Zarębski, Rozwój badań hydrogeologicznych w Centralnym Rejonie Węglowym LZW w okresie 1964-1981. Instytut Kształtowania Środowiska Lublin, GIG Oddz. Terenowy Lublin
[28] Spatial Development Plan of the Central Coal Region of the Lublin Coal Basin.
[29] Resolution of the Council of Ministers no. 58/77 on the construction of a pilot-mining mine in the LZW, (1977).
[30] Resolution of the Council of Ministers no. 34/88 on the suspension of the construction of the k-2 mine in Stefanów, (1988).
[31] Resolution of the Sejm of the Polish People’s Republic of December 18, 1976 on the five-year national socioeconomic plan for the years 1976-1980. Journal of Laws of 1976 no. 39, item 226.
[32] Resolution of the Council of Ministers no. 7/89 on suspension of financing the construction of the Bogdanka mine from central funds, (1989).
[33] Regulation No. 10 of the Minister of Local Economy and Environmental Protection of January 20, 1974, on the establishment of a technical standard for the design of multi-family dwellings and residential buildings for nonagricultural people, „Dziennik Budownictwa“ (1974).

Authors and Affiliations

Michał Tomasz Dmitruk

1

e-mail:

ORCID:

Lublin University of Technology, 38D Nadbystrzycka Str., 20-618 Lublin, Poland

Changes of springs’ yield of Lublin Upland and Roztocze Region in 1998–2008

Zdzisław Michalczyk Stanisław Chmiel Sławomir Głowacki Beata Zielińska

Journal of Water and Land Development | 2008 | No 12 | 113-125

Keywords springs yield irregularity of yield Lublin Upland and Roztocze Region

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Abstract

Lublin Upland and Roztocze region are known for the occurrence of a large number of springs of high yield. These springs are fed mainly from Cretaceous or Tertiary water-bearing horizon. In order to determine variability of springs’ yield, 61 selected springs were analysed in spring periods of the years 1998–2008. Collected hydrometric materials allowed for comparing average and extreme yield values of springs in various physiographic regions within the period of 11 years. Average value was 76.1 dm3·s–1, while the mean of the minimal yields was 44.7 dm3·s–1 and of the maximal – 132.7 dm3·s–1. Coefficient of irregularity of the springs’ yield ranged from 1.5 to 5.0, which may lead to the conclusion that the springs’ yield is constant or varies slightly. In some cases the irregularity was higher but it was determined by hydrogeological, meteorological and local factors.

Authors and Affiliations

Zdzisław Michalczyk

Stanisław Chmiel

Sławomir Głowacki

Beata Zielińska

The squamation of “Ctenacanthus” costellatus (Chondrichthyes: Ctenacanthiformes) from the Carboniferous of Lublin area, south-eastern Poland

Michał Ginter Stanisław Skompski

Acta Geologica Polonica | 2019 | vol. 69 | No 4 | 571-582 | DOI: 10.24425/agp.2019.126440

Keywords Ctenacanthiformes Sharks Dermal skeleton Viséan Lublin Coal Basin

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Abstract

A sample of late Viséan limestone from the Włodawa IG-4 borehole, east of Lublin, Poland, yielded a piece of a tooth and a few hundred well-preserved scales comparable to those of “Ctenacanthus” costellatus Traquair, 1884 from Glencartholm, Scotland, UK. Most of the scales are typical compound body scales of the ctenacanthid type. Their crowns are composed of several separate odontodes whose distal ends are turned backwards and bases are characterised by concave undersides. In the material, there are also sparse scales with similar crowns but with flat or convex bulbous bases, as well as ornamented plates and single, star-like denticles, probably from the head region. The taxonomic status of “Ctenacanthus” costellatus was analysed and a new generic name for that species, viz. Glencartius gen. nov., is proposed.

Authors and Affiliations

Michał Ginter

Stanisław Skompski

Characteristics of 13th-century mortars from the tower at Lublin Castle

Beata Klimek

Archives of Civil Engineering | 2023 | vol. 69 | No 2 | 83-95 | DOI: 10.24425/ace.2023.145254

Keywords historical mortars from the 13th century research Lublin castle tower

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Abstract

The tower at Lublin Castle, known as the donjon, is the only monument of Romanesque art on the eastern side of the Vistula River. The cylindrical, brick building is part of the Lublin Castle complex. During contemporary restoration work, the 13th-century walls were uncovered, making it possible to retrieve the original materials. The article presents the mineralogical, chemical and granulometric characteristics. The analytical methodology included: qualitative mineralogical analysis of the whole sample by X-ray diffraction (XRD); morphological studies with elemental evaluation and microanalysis of the binder by scanning electron microscopy and energy-dispersive X-ray spectroscopy (SEM-EDS). Residue determination of hydrochloric acid-insoluble parts and their granulometric analysis were performed. This methodology enabled to determine the composition of the mortars. It was found that the tested mortars have a similar mineralogical structure, but slightly differ in the proportion of individual components, primarily aggregate fractions. The samples consist mainly of quartz, calcite, and silicates. Moreover, the lime binder of the mortars was shown to be microcrystalline in nature. The aggregate used in historical mortars predominantly consisted of quartz sand and minerals of the feldspar and silicate group. The condition of the mortars requires conservation interventions. The performed characterization of the historic mortars was important for designing compatible restoration mortars.

Authors and Affiliations

Beata Klimek

1

e-mail:

ORCID:

Lublin University of Technology, Faculty of Civil Engineering and Architecture, Department of Conservation and Built Heritage, Nadbystrzycka St. 40, 20-618 Lublin, Poland

The use of non-invasive ERT method to diagnose karst in roadengineering in the Lublin Upland (Poland)

Maciej Maślakowski Anna Lejzerowicz Grzegorz Pacanowski Rafał Kuszyk

Archives of Civil Engineering | 2024 | vol. 70 | No 1 | 557-571 | DOI: 10.24425/ace.2024.148928

Keywords carbonate rocks ERT (Electrical Resistivity Tomography) karst Lublin Upland Poland

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Abstract

Appropriate design in linear construction depends on many factors, including detailed geological conditions. One of the biggest problems are unrecognized erosion forms, in particular karst ones, which have a huge impact on the design and subsequent operation of roads. For this purpose, in addition to conventional methods such as drilling or geotechnical probing, which are point-based, non-invasive spatial geophysical methods are used. This article presents an example of the use of geoelectrical surveys, Electrical Resistivity Tomography (ERT) for the recognition of karst zones for linear investments. The article describes ERT investigations, which to some extent allows to identify dangerous karst phenomena occurring in the Lublin Upland (Poland), which are of great importance at the design stage of roads and in their further safe operation. Non-invasive geophysical research has been verified and confirmed by traditional geotechnical research, which confirms the effectiveness of their use. The Electrical Resistivity Tomography was used as a method providing a broader spectrum of knowledge on the spatial arrangement of soil layers in the subgrade of the planned road investments. It also enabled a more accurate, more detailed interpretation of geotechnical studies. The described geophysical investigations opens wide possibilities for their application to researchers. In the future, non-invasive methods have a chance to become as reliable as geotechnical methods, but this requires a lot of research to improve the effectiveness and accuracy of the interpretation of the obtained results.

Authors and Affiliations

Maciej Maślakowski

1

e-mail:

ORCID:

Anna Lejzerowicz

1

e-mail:

ORCID:

Grzegorz Pacanowski

1

e-mail:

ORCID:

Rafał Kuszyk

2

e-mail:

ORCID:

Warsaw University of Technology, Faculty of Civil Engineering, Al. Armii Ludowej 16, 00-637 Warsaw, Poland
Polish Geological Institute – National Research Institute, Rakowiecka 4, 00-975 Warsaw, Poland

Hydrological changes in the Lublin Polesie during the Late Glacial and Holocene as reflected in the sequences oflacustrine and mire sediments

Krystyna Bałaga

Studia Quaternaria | 2002 | Vol.19 | 37-53

Keywords Lublin Polesie Late Glacial Holocene hydrological changes pollen analysis

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Abstract

The paleoecological research of biogenie sediments sampled in the different lake-mire ecosystems of the ŁęcznaWłodawa Lake District were the basis of studies on hydrological changes during the Late Glacial and Holocene. The lithological differentiation (spatial and temporal) of lacustrine and mire sediments in the studied sites indicates that the hydrological changes were of local nature. The investigations also evidence a specific functioning of the lakes in this region. Lake basins were formed as a result of the ground ice degradation and the transformation of groundwater circulation in the Late Glacial. The total area of lakes in the Lake District was the largest from the Younger Dryas to the Subboreal chronozone. The gradual lowering ofwater level during the early Holocene resulted in the transformation of sedimentation process, and in the development of typologically differentiated mires and lacustrinc-mire complexes

Authors and Affiliations

Krystyna Bałaga

Sub-Permian basement in the Radom-Lublin area – geological and reservoir implications based on seismic geophysical data

Lidia Dziewińska Radosław Tarkowski

Gospodarka Surowcami Mineralnymi - Mineral Resources Management | 2022 | vol. 38 | No 2 | 207-228 | DOI: 10.24425/gsm.2022.141661

Keywords Radom-Lublin area subsoil geology effective reflection coefficients (ERC) hydrocarbon reservoirs seismic

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Abstract

This paper presents the results of an analysis of selected seismic profiles (reflection and refraction data) from the Radom-Lublin area aimed at obtaining a better understanding of geological structure and the identification of hydrocarbon deposits. To accurately reproduce the seismic reflection covering the sub-Permian formations, seismic cross sections were interpreted based on effective reflection coefficients (ERC). In interpreting the results, reference was made to the results of studies of the area using other geophysical methods.
The results of these studies made it possible to obtain new information on the geology and structure of the Paleozoic complex of the Radom-Lublin area and its relationships with the basement tectonics. The structural arrangement of Carboniferous and Devonian formations as well as older Silurian, Ordovician, and Cambrian series were recognized. Selected significant tectonic and lithological discontinuities and the nature and directions of their course were characterized. Special attention was given to regional tectonic zones: the Skrzynno Fault, the Ursynów-Kazimierz fault zone and the Kock zone. The use of ERC methodology made it possible to define the boundaries of lithostratigraphic units in Carboniferous, Devonian, and older formations. The obtained results can be used to assess hydrocarbon accumulation in the area under consideration.

Authors and Affiliations

Lidia Dziewińska

1

e-mail:

ORCID:

Radosław Tarkowski

1

e-mail:

ORCID:

Mineral and Energy Economy Research Institute, Polish Academy of Sciences, Kraków, Poland

A putative Tournaisian and Visean volcanic-sedimentary succession in the Lublin Basin, SE Poland: depositional processes, petrological characteristics and sequence stratigraphy

Maria I. Waksmundzka Aleksandra Kozłowska Magdalena Pańczyk

Acta Geologica Polonica | vol. 71 | No 3 | 305-344 | DOI: 10.24425/agp.2020.134559

Keywords Tournaisian Visean Lublin Basin Sequence stratigraphy Petrography Cyclothems Volcanic source areas

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Abstract

The aim of this study was to establish the stratigraphic extent of a putative Tournaisian Stage within the Carboniferous succession in the Lublin Basin. The oldest part of the succession, known as the Huczwa Formation and comprising depositional sequences 1–4, was investigated based on lithofacies analysis, sequence stratigraphy and petrographic studies. The article provides descriptions of depositional sequences, parasequences (cyclothems) and lithofacies that were formed in a range of environments (elements of depositional architecture) and as a result of volcanic processes – lava and pyroclastic eruptions and chemical weathering of their products. Correlation of the sequence stratigraphy to the West European and global Carboniferous chronostratigraphic divisions, as well as to the Khoriv suite in the Lviv-Volyn Basin in adjacent Ukraine, indicates a putative late Tournaisian age for sequence 1, and a late Visean age for sequences 2–4. There is a stratigraphic gap between sequences 1 and 2, spanning probably the uppermost Tournaisian and the lower and middle Visean. The upper Tournaisian is represented by the FRST-LST deposits of sequence 1, comprising mainly volcaniclastic conglomerates and sandstones developed in braided-river channels and incised valleys with hyperconcentrated flow processes. These deposits are represented by polymictic paraconglomerate and lithic/sublithic/subarkose arenites or sublithic wackes, and contain predominantly grains of acidic and alkaline volcanic and igneous rocks. This material probably came from the Łuków-Wisznice Elevation and the Volynian Polesia region, located to the NE and E of the Lublin Basin. In the uppermost part of sequence 1, volcanic rocks and tuffs appear which developed during the activity of at least three volcanic cones in the Lublin Basin. The volcanoes were the source of alkaline lavas in the central and SW areas of the basin, and of acidic lavas in the SE area, previously undescribed. The Visean sequences 2–4 consist of the FRST-LST sediments deposited within incised valleys. The TST and HST deposits accumulated mainly in a shallow ramp-type carbonate shelf, shallow clayey shelf and deltaic environments.

Bibliography

Al-Mashaikie, S.Z.A.K. and Al-Hawbanie, A.M. 2010. Petrography and geochemical study of the Perlite Rocks from Bait Al-Qeyarie, Kawlan Area, Yemen. Earth Science, 21 (2), 195–217.
Arnott, R.W.C and Hand, B.M. 1989. Bedforms, primary structures and grain fabric in the presence of suspended sediment rain. Journal of Sedimentary Petrology, 59 (6), 1062–1069.
Ashley, G.M. and Sheridan, R.E. 1994. Depositional model for valley fills on a passive continental margin. In: Dalrymple, R.W., Boyd, R. and Zaitlin, B.A. (Eds), Incised-Valley Systems: Origin and Sedimentary Sequences. Society of Economic Paleontologists and Mineralogists Special Publication, 51, 285–301. Tulsa, Oklahoma.
Baldwin, B. and Butler, C.O. 1985. Compaction Curves. American Association of Petroleum Geologists Bulletin, 69 (4), 622–626.
Batalla, R.J., De Jong, C., Ergenzinger, P. and Sala, M. 1999. Field observations on hyperconcentrated flows in mountain torrents. Earth Surface Processes and Landforms, 24, 247–253.
Bojkowski, K. and Dembowski, Z. 1988. Paleogeography of Carboniferous in the Lublin Coal Basin at the background of paleogeography of Carboniferous in Poland. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 18–26; 227–228.
Bojkowski, K. and Musiał, Ł. 1978. Stratygrafia makrofaunistyczna karbonu. In: Niemczycka, T. (Ed.), Profile Głębokich Otworów Wiertniczych Instytutu Geologicznego, 45, 129–131.
Catuneanu, O. 2006. Principles of Sequence Stratigraphy, 375 pp. Elsevier; Amsterdam.
Cebulak, S. 1988a. Petrographic characteristics of Carboniferous deposits. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 77–88; 231–232. [In Polish with English summary]
Cebulak, S. 1988b. Geological outline of sub-Carboniferousbasement. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 31–34. [In Polish with English summary]
Cebulak, S. 1989. Badania petrograficzne osadów karbonu. In: Krassowska, A. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 66, 180–189.
Cebulak, S., Porzycki, J., Laskowski, M., Różkowski, A., Rudzińska, T., Szewczyk, J., Karwasiecka, M. and Waksmundzka, M.I. 2011. Badania surowcowe boksytów i węgli występujących w utworach karbonu. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 130, 116–122. [In Polish with English summary]
Coleman, J.M. and Wright, L.D. 1975. Modern river deltas: variability of processes and sand bodies. In: Broussard, M. L. (Ed.), Deltas, models for exploration, 99–150. Houston Geological Society; Houston.
Davydov, V.I., Korn, D. and Schmitz, M.D. 2012. The Carbonifeous Period. In: Gradstein, F.M., Ogg, J.G., Schmitz, M.D. and Ogg, G.M. (Eds), The Geologic Time Scale, 603–651. Elsevier, Amsterdam.
Depciuch, T. 1974. Rocks of the Precambrian Platform in Poland. Part 2 – Sedimentary cover. In: Łaszkiewicz, A. (Ed.), Prace Instytutu Geologicznego, 74, 81–83. [In Polish with English summary]
Duff, McL.D. and Walton, E.K. 1962. Statistical basis for cyclothems: a quantitative study of the sedimentary succession in the East Pennine Coalfield. Sedimentology, 1 (4), 235–255.
Einsele, G. 1992. Sediment of Marine Delta Complexes, Depositional Rhythms and Cyclic Sequences. In: Einsele, G. (Ed.), Sedimentary Basins. Evolution, Facies and Sediment, 147– 160; 271–310. Springer-Verlag; Berlin, Heidelberg.
Elliott, T. 1974. Interdistributary bay sequence and their genesis. Sedimentology, 21 (4), 611–622.
Elliott, T. 1975. The sedimentary history of a delta lobe from a Yoredale (Carboniferous) cyclothem. Proceedings of the Yorkshire Geological Society, 40 (4), 505–536.
Elliott, T. 1976a. Sedimentary sequences from the Upper Limestone Group of Northumberland. Scottish Journal of Geology, 12 (2), 115–124.
Elliott, T. 1976b. Upper Carboniferous sedimentary cycles produced by river-dominated, elongate deltas. Journal of the Geological Society of London, 132, 199–208.
Elliott, T. 1978. Deltas. In: Reading, H.G. (Ed.), Sedimentary envinronments and facies, 97–142. Blackwell Scientific Publications; Oxford.
Fisher, R.V. and Schmincke, H.U. 1984. Pyroclastic rocks, 471 pp. Springer-Verlag; Berlin, Heidelberg, New York, Tokyo.
Flügel, E. 2004. Depositional Models. Facies Zones and Standard Microfacies. In: Flügel, E. (Ed.), Microfacies of Carbonate Rocks Analysis, Interpretation and Application, 657–723. Springer-Verlag; Berlin, Heidelberg.
Francis, P. and Oppenheimer, C. 2004. Volcanoes, 536 pp. Oxford University Press; Oxford.
Galets’kyi, L.S. 2007. An Atlas of the Geology and Mineral Deposits of Ukraine 1:5 000 000. Section IV. Geological slice maps: Pre-Carboniferous. National Academy of Science of Ukraine; Kyiv and Toronto.
Gastaldo, R., Denko, T. and Liu, Y. 1993. Application of sequence and genetic stratigraphic concepts to carboniferous coal-bearing strata: an example from the Black Warrior Basin, USA. Geologische Rundschau, 82 (2), 212–226.
Godyń, K. 2011. Volcaniclasts of Lower Carboniferous rock formations in Western Pomerania. Biuletyn Państwowego Instytutu Geologicznego, 444, 55–64. [In Polish with English summary]
Grocholski, A. and Ryka, W. 1995. Carboniferous magmatism of Poland. In: Zdanowski, A. and Żakowa, H. (Eds), The Carboniferous System in Poland. Prace Państwowego Instytutu Geologicznego, 148, 181–190.
Hajdenrajch, M. 2010. Stratygrafia sekwencji i sedymentacja utworów karbonu rejonu Niedrzwicy (płd.-zach. Lubelszczyzna), 68 pp. Unpublished M.Sc. thesis, University of Warsaw; Warszawa.
Hampson, G., Stollhofen, H. and Flint, S. 1999. A sequence stratigraphic model for the Lower Coal Measures (Upper Carboniferous) of the Ruhr district, north-west Germany. Sedimentology, 46 (6), 1199–1231.
Hein, F.J. and Walker, R.G. 1977. Bar evolution and development of stratification in the gravelly, braided, Kicking Horse River, British Columbia. Canadian Journal of Earth Sciences, 14 (4), 562–570.
Helland-Hansen, W. 2009. Towards the standardization of sequence stratigraphy. Earth-Science Reviews, 94, 95–97.
Helland-Hansen, W. and Gjelberg, J.G. 1994. Conceptual basis and variability in sequence stratigraphy: a different perspective. Sedimentary Geology, 92 (1–2), 31–52.
Jaworowski, K., 1987. Kanon petrograficzny najczęstszych skał osadowych. Przegląd Geologiczny, 35 (4), 205–209.
Kędzior, A., 2016. Reconstruction of an Early Pennsylvanian fluvial system based on geometry of sandstone bodies and coal seams: the Zabrze Beds of the Upper Silesia Coal Basin, Poland. Annales Societatis Geologorum Poloniae, 86 (4), 437–472.
Kmiecik H., 1988. Miospore stratigraphy of the Carboniferous deposits. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 131–141; 235–237. [In Polish with English summary]
Kmiecik, H. and Trzepierczyńska, A. 2007. Wyniki badań palinologicznych utworów karbonu. In: Waksmundzka, M.I. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 119, 119–126. [In Polish with English summary]
Korejwo, K. 1974. The Carboniferous of the Abramów structure. Acta Geologica Polonica, 24 (4), 631–661. [In Polish with English summary]
Korejwo, K. 1986. Biostratigraphy of the Carboniferous deposits of the Świdnik blocks (Lublin Coal Basin). Acta Geologica Polonica, 36 (4), 337–346.
Korejwo, K. and Teller, L. 1968. The Carboniferous of the western part of the Lublin Basin. Acta Geologica Polonica, 18 (1), 154–177. [In Polish with English summary]
Korejwo, K. and Teller, L. 1972. The Carboniferous of the Kock elevation. Acta Geologica Polonica, 22 (4), 655–675. [In Polish with English summary]
Kostyk, I.O., Matrofailo, M.M., Lelyk, B.I. and Korol, M.D. 2016. New data about sequence formation, compound and capacity of the coal-bearing formation of Carbon of the Lviv-Volyn Basin. Naukovyi visnik NGU, 1 (1), 19–31.
Kozłowska, A. and Waksmundzka, M.I. 2020. Diagenesis, sequence stratigraphy and reservoir quality of the Carboniferous deposits of the southeastern Lublin Basin (SE Poland). Geological Quarterly, 64 (2), 422–459.
Krassowska, A. (Ed.) 1989. Profile głębokich otworów wiertniczych Państwowego Instytutu Geologicznego, 66, 1–250.
Krzywiec, P. 2007. Tectonics of the Lublin area (SE Poland) – new views based on results of seismic data interpretation. Biuletyn Państwowego Instytutu Geologicznego, 422, 1–18.
Krzywiec, P., Mazur, S., Gągała, Ł., Kufrasa, M., Lewandowski, M., Malinowski, M. and Buffenmyer, V. 2017. Late Carboniferous thin-skinned compressional deformation above the SW Edge of the East European craton as revealed by seismic reflection and potential field data – Correlation with the Variscides and the Appalachians. In: Law, R.D., Thigpen, J.R., Merschat, A.J. and Stowell, H.H. (Eds), Linkages and Feedbacks in Orogenic Systems. Geological Society of America Memoir, 213, 353–372.
Krzywiec, P. and Narkiewicz M., 2003. O stylu strukturalnym kompleksu dewońskokarbońskiego Lubelszczyzny w oparciu o wyniki interpretacji danych sejsmicznych. Przegląd Geologiczny, 51 (9), 795–797.
Kufrasa, M., Stypa, A., Krzywiec, P. and Słonka, Ł., 2019. Late Carboniferous thin-skinned deformation in the Lublin Basin, SE Poland: results of combined seismic data interpretation, structural restoration and subsidence analysis. Annales Societatis Geologorum Poloniae, 89 (2), 175–194.
Le Maitre, R. W., Bateman, P., Dudek, A., Keller, J., Lameyre, J., Le Bas, M. J., Sabine, P.A., Schmid, R., Sørensen, H., Streckeisen, A., Wooley, A.R. and Zanettin, B. 1989. A classification of ignous rocks and glossary of terms: Recommendations of the International Union of Geological Sciences Subcommision on the Systematic of Ignous Rocks. Blackwell Scientific Publications, Oxford.
Łydka, K. 1996. Diageneza wulkanoklastyków. Przegląd Geologiczny, 44 (6), 619–620.
Martinsen, O.J. 1994. Evolution of an incised-valley fill, the Pine Ridge Sandstone of Southeastern Wyoming, U.S.A.: systematic sedimentary response to relative sea-level change, In: Dalrymple, R.W., Boyd, R. and Zaitlin, B.A. (Eds), Incised-valley Systems: Origin and Sedimentary Sequences. Society of Economic Paleontologists and Mineralogists Special Publication, 51, 109–128.
Matyja, H. 2008. Pomeranian basin (NW Poland) and its sedimentary evolution during Mississippian times. Geological Journal, 43 (2-3), 123–150.
Mazur, S., Aleksandrowski, P., Kryza, R. and Oberc-Dziedzic T. 2006. The Variscan orogen in Poland. Geological Quarterly, 50 (1), 89–119.
Mazur, S., Aleksandrowski, P., Turniak, K., Krzemiński, L., Mastalerz, K., Górecka-Nowak, A., Kurowski, L., Żelaźniewicz, A. and Fanning, M.C. 2010. Uplift and late orogenic deformation of the Central European Variscan belt as revealed by sediment provenance and structural record in the Carboniferous foreland basin of western Poland. International Journal of Earth Sciences, 99 (1), 47–64.
Miall, A.D. 1977. A Review of the braided-river depositional environment. Earth Science Reviews, 13 (1), 1–62.
Miall, A.D. 1978. Lithofacies types and vertical profile models in braided river deposits: a summary. In: Miall, A.D. (Ed.), Fluvial sedimentology. Canadian Society of Petroleum Geologists Memoir, 5, 597–604.
Miall, A.D. 1986. Deltas. In: Walker, R.G. (Ed.), Facies Models 2nd Edition, Geoscience Canada Reprint Series 1, 105–118.
Miall, A.D. 1996. The Geology of Fluvial Deposits Sedimentary Facies, Basin Analysis, and Petroleum Geology, 26–30; 40–41. Springer; Berlin, Heidelberg.
Michum, Jr R.M. 1977. Seismic Stratigraphy and Global Changes of Sea Level, Part 11: Glossary of Terms used in Seismic Stratigraphy: Section 2. Application of Seismic Reflection Configuration to Stratigraphic Interpretation. In: Payton, E. (Ed) Seismic Stratigraphy – Applications to Hydrocarbon Exploration. American Association of Petroleum Geologists Memoir, 26, 205–212.
Miłaczewski, L. 2010. Subcrop map of the sub-Carboniferous unconformity. In: Modliński Z. (Ed.), Paleogeological Atlas of the sub-Permian Paleozoic of the East-European Craton in Poland and neighbouring areas. PIG-PIB; Warszawa. [In Polish with English summary]
Miłaczewski, L. and Niemczycka, T. 1967. Geological structure of the Niedrzwica region. Kwartalnik Geologiczny, 11 (3), 557–571. [In Polish with English summary]
Migier, T. 1988. Macrofloral stratigraphy of the Carboniferous deposits. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 120–131; 234–235. [In Polish with English summary]
Musiał, Ł. and Tabor, M. 1979. Stratygrafia karbonu Lubelskiego Zagłębia Węglowego na podstawie makrofauny. In: Migier, T. (Ed.), Stratygrafia Węglonośnej Formacji Karbońskiej w Polsce, II Sympozjum Sosnowiec, 4–5 maja 1977, 35–43. Wydawnictwa Geologiczne; Warszawa.
Musiał, Ł. and Tabor, M. 1988. Macrofaunal stratigraphy of Carboniferous. In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 88–122; 232–233. [In Polish with English summary]
Musiał, Ł. and Tabor, M. 1989. Stratygrafia karbonu na podstawie makrofauny. In: Krassowska, A. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 66, 105–108.
Muszyński, A., Biernacka, J., Lorenc, S., Protas, A., Urbanek, Z. and Wojewoda, J. 1996. Petrology and a depositional environment of Lower Carboniferous rocks near Dygowo and Kłanino (the Koszalin-Chojnice zone). Geologos, 1, 93–126. [In Polish with English summary]
Narkiewicz, M. 2007. Development and inversion of Devonian and Carboniferous basins in the eastern part of the Variscan foreland (Poland). Geological Quarterly, 51 (3), 231–256.
Narkiewicz, M. 2020. The Variscan foreland in Poland revisited: new data and new concepts. Geological Quarterly, 64 (2), 377–401.
Narkiewicz, M., Miłaczewski, L., Krzywiec, P. and Szewczyk, J. 1998. Outline of the Devonian depositional architecture in the Radom-Lublin area. In: Narkiewicz, M. (Ed.), Sedimentary basin analysis of the Polish Lowlands. Prace Państwowego Instytutu Geologicznego, 165, 57–72.
Nemec, W. and Postma, G. 1993. Quaternary alluvial fans in south-western Crete: sedimentation processes and geomorphic evolution. In: Marzo, M. and Puigdefabregas, C. (Eds), Alluvial Sedimentation. International Association of Sedimentologists, Special Publication, 17, 235–276.
Nemec, W. and Steel, R.J. 1984. Alluvial and coastal conglomerates: their significant features and some comments on gravelly mass-flow deposits. In: Koster, E.H. and Steel, R.J. (Eds), Sedimentology of Gravels and Conglomerates. Canadian Society of Petroleum Geologists Memoir, 10, 1–31.
Niemczycka, T. (Ed.) 1978. Profile Głębokich Otworów Wiertniczych Instytutu Geologicznego, 45, 1–292.
Nosova, A.A., Veretennikov, N.V. and Levskii, L.K. 2005. Nature of the mantle source and specific features of crustal contamination of Neoproterozoic flood basalts of the Volhynia Province (Nd-Sr Isotopic and ICP-MS Geochemical Data). Doklady Earth Sciences, 401A, 429–433. Translated from Doklady Earth Sciences, 401, 521–525.
Pańczyk, M. and Nawrocki, J. 2015. Tournaisian 40Ar/39Ar age from alkaline basalts from the Lublin Basin (SE Poland). Geological Quarterly, 59 (3), 473–478.
Pettijohn, F.J., Potter, P.E. and Siever, R. 1972. Sand and Sandstone, 583 pp. New York, Springer.
Popek, T., 1986. Przejawy wulkanizmu w górnym wizenie na obszarze lubelskim. Przegląd Geologiczny, 4, 212–215.
Porzycki, J. 1979. Litostratygrafia osadów karbonu Lubelskiego Zagłębia Węglowego. In: Migier, T. (Ed.), Stratygrafia węglonośnej formacji karbońskiej w Polsce. II Sympozjum, Sosnowiec, 19–27. Wydawnictwa Geologiczne; Warszawa.
Porzycki, J. 1988. History of geological survey and discovery of the Lublin Coal Basin. Lithologic and sedimentologic characteristics of Carboniferous deposits, In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 9–18; 40–76; 226–227; 229–231. [In Polish with English summary]
Porzycki, J. and Zdanowski, A. 1995. Southeastern Poland (Lublin Carboniferous Basin), In: Zdanowski, A. and Żakowa, H. (Eds), The Carboniferous System in Poland. Prace Państwowego Instytutu Geologicznego, 168, 102–109.
Postma, G. 1990. An analysis of the variation in delta architecture. Terra Nova, 2 (2), 124–130.
Posamentier, H.W. and Allen, G.P. 1999. Siliciclastic Sequence Stratigraphy: Concepts and Applications. Society of Economic Paleontologists and Mineralogists Concepts in Sedimentology and Paleontology, 7, 1–210.
Posamentier, H.W., Jervey, M.T. and Vail, P.R. 1988. Eustatic controls on clastic deposition. I – conceptual framework. In: Wilgus, C.K., Hastings, B.S., Kendall, C.G.S.C., Posamentier, H.W., Ross, C.A. and Van Wagoner, J.C. (Eds), Sea-Level Changes: An Integrated Approach. Society of Economic Paleontologists and Mineralogists Special Publication, 42, 110–124.
Porębski, S.J. and Steel R.J. 2003. Shelf-margin deltas: their stratigraphic significance and relation to deepwater sands. Earth-Science Reviews, 62, 283–326.
Pożaryski, W. and Dembowski, Z. 1983. Geological Map of Poland and Neighbouring Countries without Cenozoic, Mesozoic and Permian Deposits. Warszawa, Poland, Geological Instytute, scale 1:1,000,000.
Pulham, A.J. 1989. Controls on internal structure and architecture of sandstone bodies within Upper Carboniferous fluvial- dominated deltas, County Clare, western Ireland. In: Whateley, M.K.G. and Pickering, K.T. (Eds), Deltas: Sites and Traps for Fossil Fuels. Geological Society Special Publication, 41, 179–203. Ramsbottom, W.H.C. 1977. Major cycles of transgression and regression (mesothems) in the Namurian. Proceedings of the Yorkshire Geological Society, 41 (3), 261–291.
Ramsbottom, W.H.C. 1978. Namurian mesothems in South Wales and northern France. Journal of the Geological Society, 135 (3), 307–312.
Reading, H.G. 1978. Facies. In: Reading, H.G. (Ed.), Sedimentary Environments and Facies, 4–14. Blackwell Science; Oxford.
Rottella, M. and Simandl, G.J. 2004. Marilla perlite – volcanic glass occurrence, British Columbia, Canada. In: Simandl, G.J., McMillan, W.J. and Robinson, N. (Eds), British Columbia Ministry of Energy Mines and Petroleum Resources, Paper 2004-2, 265–272. Geological Survey Branch; Victoria.
Rust, B.R. 1978. A classification of alluvial channel systems. In: Miall, A.D. (Ed.), Fluvial Sedimentology. Canadian Society of Petroleum Geologists Memoir, 5, 187–198.
Ryka, W. and Maliszewska, A. (Eds) 1991. Słownik petrograficzny. II wyd., 415 pp. Wydawnictwa Geologiczne; Warszawa.
Scruton, P.C. 1960. Delta building and the deltaic sequence. In: Shepard, F.P., Phleger, F.B. and Angel, T.H. (Eds), Recent sediments, northwest Gulf of Mexico, 82–102. American Association of Petroleum Geologists Special Publication; Tulsa.
Segerstrom, K. 1950. Erosion studies of Paricutin, State of Michoacan, Mexico. U. S. Geological Survey Bulletin, 965-A, 1–164.
Shulga, V.F., Zdanovski, A., Zayceva, L.B., Yvanova, A.V., Yvanyna, A.V., Korol, N.D., Kotasova, A., Kotas, A., Kostyk, I.O., Lelyk, B.I., Migier, T., Manycev, B.Y., Matrofailo, M.M., Ptak, B., Savcuk, V.S., Sedayeva, G.M. and Stepanenko, J.G. 2007. Correlation of the Carboniferous coal-bearing formations of the Lviv-Volyn and Lublin Basins, 428 pp. National Academy of Sciences of Ukraine Institute of Geological Sciences Polish State Geological Institute Upper Silesian Branch; Kiev. [In Russian with English and Polish summaries]
Shumlyanskyy, L.V. 2014. Geochemistry of the Osnisk-Mikashevichy Volcanoplutonic Complex of the Ukrainian Shield. Geochemistry International, 52 (11), 912–924.
Siemaszko, E. 1978. Permian effusive rocks from SW part of the Fore-Sudetic Monocline. Kwartalnik Geologiczny, 22 (3), 571–590. [In Polish with English summary]
Skompski S. 1988. Limestone microfacies and facies position of Upper Visean sediments in north-eastern part of the Lublin Coal Basin. Przegląd Geologiczny, 36 (1), 25–30. [In Polish with English summary]
Skompski, S. 1995. Succession of limestone microfacies as a key to the origin of the Yoredale-type cyclicity (Viséan/ Namurian, Lublin Basin, Poland). XIII International Congress Carboniferous–Permian, Kraków, Abstracts, 133.
Skompski, S. 1996. Stratigraphic position and facies significance of the limestone bands in the subsurface Carboniferous succession of the Lublin Upland. Acta Geologica Polonica, 46 (3), 171–268.
Skompski, S. 1998. Regional and global chronostratigraphic correlation levels in the late Visean to Westphalian succession of the Lublin Basin (SE Poland). Geological Quarterly, 42, 121–130.
Skompski, S. 2011. Wykształcenie facjalne wapieni dolnokarbońskich w rejonie otworu Parczew IG 10. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 130, 111–116. [In Polish with English summary]
Skompski, S. and Soboń-Podgórska, J. 1980. Foraminifers and conodonts in the Viséan deposits of the Lublin Upland. Acta Geologica Polonica, 30, 87–96.
Smith, D.G. 1983. Anastomosed fluvial deposits: modern examples from Western Canada. In: Collinson, J. and Lewin, J. (Eds), Modern and Ancient Fluvial Systems. Special Publication of the International Association of Sedimentologists, 6, 155–168.
Soboń-Podgórska, J. 1988. Microfaunal stratigraphy of the Carboniferous deposits (foraminifers). In: Dembowski, Z. and Porzycki, J. (Eds), Carboniferous of the Lublin Coal Basin. Prace Instytutu Geologicznego, 122, 112–120; 233– 234. [In Polish with English summary]
Soboń-Podgórska, J. and Tomaś, A. 1995. Foraminifera. In: Zdanowski, A. and Żakowa, H. (Eds), The Carboniferous System in Poland. Prace Państwowego Instytutu Geologicznego, 148, 44–47.
Svendsen, J., Stollhofen, H., Krapf, C.B.E. and Stanistreet, I.G. 2003. Mass and hyperconcentrated flow deposits record dune damming and catastrophic breakthrough of ephemeral rivers, Skeleton Coast Erg, Namibia. Sedimentary Geology, 160 (1-3), 7–31.
Szulczewski, M., Bełka, Z. and Skompski, S. 1996. The drowning of carbonate platform: an example from the Devonian– Carboniferous of the southwestern Holy Cross Mountains, Poland. Sedimentary Geology, 106 (1-2), 21–49.
Środoń, J., Paszkowski, M., Drygant, D., Anczkiewicz, A. and Banaś, M. 2013. Thermal history of Lower Paleozoic rocks on the Peri-Tornquist margin of the East European Craton (Podolia, Ukraine) inferred from combined XRD, K-Ar, and AFT data. Clays and Clay Minerals, 61 (2), 107–132.
Tomaszczyk, M. and Jarosiński, M. 2017. The Kock Fault Zone as an indicator of tectonic stress regime changes at the margin of the East European Craton (Poland). Geological Quarterly, 61, 908–925.
Tunbridge, I.P. 1981. Sandy high-energy flood sedimentation – some criteria for recognition, with an example from the Devonian of SW England. Sedimentary Geology, 28 (2), 79–95.
Turner, B.R. and Whateley, M.K.G. 1983. Structural and sedimentological controls of coal deposition in the Nongoma graben, northern Zululand, South Africa. In: Collinson, J.D. and Lewin, J. (Eds), Modern and ancient fluvial systems. Special Publication of the International Association of Sedimentologists, 6, 457–471. Vail, P.R., Todd, R.G. 1981. Northern North Sea Jurassic unconformities, chronostratigraphy and sea-level changes from seismic stratigraphy. In: Illing, L.V. and Hobson, G.D. (Eds), Petroleum Geology of the Continental Shelf of North West Europe, 216–235. Heyden and Son Ltd.; London.
VanWagoner, J.C. 1985. Reservoir facies distribution as controlled by sea-level change. Society of Economic Paleontologists and Mineralogists Mid-Year Meeting Abstracts, Golden, Colorado, August 11–14, 91–92. Society of Economic Paleontologists and Mineralogists; Tulsa.
Van Wagoner, J.C., Posamentier, H.W., Mitchum, R.M. Jr, Vail, P.R., Sarg, J.F., Loutit, T.S. and Hardenbol, J. 1988. An overview of the fundamentals of sequence stratigraphy and key definitions. In: Wilgus, K., Hastings, B.S., Kendall, C.G.St.C., Posamentier, H.W., Ross, C.A. and Van Wagoner, J.C. (Eds), Sea-Level Changes – An Integrated Approach. Society of Economic Paleontologists and Mineralogists Special Publication, 42, 39–45.
Waksmundzka, M.I. 1998. Depositional architecture of the Carboniferous Lublin Basin. In: Narkiewicz, M. (Ed.), Sedimentary basin analysis of the Polish Lowlands. Prace Państwowego Instytutu Geologicznego, 165, 89–100. [In Polish with English summary]
Waksmundzka, M.I. 2007. Karbon. Litologia, stratygrafia i sedymentologia. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 118, 124–130. [In Polish with English summary]
Waksmundzka, M.I. 2008. Correlation and origin of the Carboniferous sandstones in the light of sequence stratigraphy and their hydrocarbon potential in the NW and Central parts of the Lublin Basin. Biuletyn Państwowego Instytutu Geologicznego, 429, 215–224. [In Polish with English summary]
Waksmundzka, M.I. 2010a. Sequence stratigraphy of Carboniferous paralic deposits in the Lublin Basin (SE Poland). Acta Geologica Polonica, 60 (4), 557–597.
Waksmundzka, M.I. 2010b. Lithofacies-paleothickness and worm’s eye maps of Carboniferous. Plates 21–24, 33–35. In: Modliński, Z. (Ed.), Paleogeological Atlas of the sub- Permian Paleozoic of the East-European Craton in Poland and neighbouring areas. PIG-PIB Warszawa. [In Polish with English summary] Waksmundzka, M.I. 2011. Karbon. Litologia, sedymentologia i stratygrafia. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 130, 101–108. [In Polish with English summary]
Waksmundzka, M.I. 2012. Braided-river and hyperconcentrated- flow deposits from the Carboniferous of the Lublin Basin (SE Poland) – a sedimentological study of core data. Geologos, 18 (3), 135–161.
Waksmundzka, M.I. 2013. Carboniferous coarsening-upward and non-gradational cyclothems in the Lublin Basin (SE Poland): palaeoclimatic implications. In: Gąsiewicz, A. and Słowakiewicz, M. (Eds), Palaeozoic Climate Cycles: Their Evolutionary and Sedimentological Impact. Geological Society, London, Special Publications, 376, 141–175.
Waksmundzka, M.I. and Buła, Z. 2020. Geological Map of Poland without Cenozoic, Mesozoic and Permian deposits 1:2,5000,000. In: Nawrocki, J. and Becker, A. (Eds), Geological Atlas of Poland, 28–29. PIG-PIB; Warszawa.
Walker, R.G. 1992. Facies, facies models, and modern stratigraphic concepts. In: Walker, R.G. and James, N.P. (Eds), Facies Models: Response to Sea Level Change, 1–14. Geological Association of Canada; St. John’s.
Walker, G.P.L. 1973. Lengths of lava flows. Philosophical Transactions of the Royal Society London, 274 (1238), 107–118.
Winchester, J.A. and Floyd, P.A. 1977. Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology, 20, 325–343.
Wiszniewska, J. and Tołkanowicz, E. 2015. Raw rock resources of the Volhynia Province during the period of Second Republic of Poland and their utilization. Przegląd Geologiczny, 63 (9), 525–530. [In Polish with English summary]
Woszczyńska, S. 2011. The Carboniferous micropalaeontology based on Foraminifera and Ostracoda. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 130, 109–110. [In Polish with English summary]
Wright, L.D. 1977. Sediment transport and deposition at river mouths: a synthesis. Geological Society of America Bulletin, 88 (6), 857–868.
Wright, LD. and Coleman, J.M. 1974. Mississippi river mouth processes: effluent dynamics and morphologic development. Journal of Geology, 82 (6), 751–778.
Zieliński, T. 1992a. Marginal moraines of NE Poland – sediments and depositional conditions. Prace Naukowe Uniwersytetu Śląskiego, 1325, 7–95.
Zieliński, T. 1992b. Proglacial valleys facies of the Silesian Upland – genetic factors and their sedimentological effects. Geologia Sudetica, 26 (1–170), 83–118.
Zieliński, T. 1995. Kod litofacjalny i litogenetyczny – konstrukcja i zastosowanie. In: Mycielska-Dowgiałło, E. and Rutkowski, J. (Eds), Badania osadów czwartorzędowych, Wybrane metody i interpretacja wyników, 220–235. Uniwersytet Warszawski; Warszawa.
Zieliński, T. 2015. Sedymentologia. Osady rzek i jezior, 594 pp. Wydawnictwo Naukowe UAM; Poznań. Żelichowski, A.M. 1969. Karbon. In: Depowski, S. (Ed.), Ropoi gazonośność obszaru lubelskiego na tle budowy geologicznej – część I: Budowa geologiczna obszaru lubelskiego. Prace Geostrukturalne Instytutu Geologicznego, 70–85.
Żelichowski, A.M. 1972. Evolution of the geological structure of the area between the Góry Świętokrzyskie and the River Bug. Biuletyn Instytutu Geologicznego, 263, 7–97; 91–97. [In Polish with English summary]
Żelichowski, A.M. 1987. Development of the Carboniferous of the SW margin of the East European Platform in Poland. Przegląd Geologiczny, 35 (5), 230–237. [In Polish with English summary]
Żelichowski, A.M. and Kozłowski, S. (Eds) 1983. Atlas of geological structure and mineral deposits in the Lublin region. Wydawnictwa Geologiczne; Warszawa. [In Polish with English summary]
Żelichowski, A.M., Porzycki, J., Cebulak, S., Musiał, Ł., Tabor, M., Migier, T. and Waksmundzka, M.I. 2011. Profil litologiczno- stratygraficzny Karbon. In: Pacześna, J. (Ed.), Profile Głębokich Otworów Wiertniczych Państwowego Instytutu Geologicznego, 130, 20–39. [In Polish with English summary]

Authors and Affiliations

Maria I. Waksmundzka

1

Aleksandra Kozłowska

1

Magdalena Pańczyk

1

Polish Geological Institute – National Research Institute, Rakowiecka 4, PL-00-975 Warsaw, Poland

Firsts Post-Tensioned Slab Bridges in Poland — the Bridge in Pawia Street in Lublin

S. Karaś

Archives of Civil Engineering | Vol. 66 | No 2 | 285-301 | DOI: 10.24425/ace.2020.131810

Keywords bridge maintenance first Polish post-tensioned concrete bridges bridges in Pawia Street in Lublin

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Abstract

The analysis was focused on three post-tensioned slab bridges, constructed in 1950s. Two of them function normally and will probably achieve the life span of 100 years required by the relevant regulations. The third one will likely be demolished soon and replaced with a new reinforced concrete frame bridge. To its degradation contributed the faulty diagnosis of its technical condition during its periodic technical inspections. The introduction briefly characterises the development of the prestressed structure theories reviewing papers on concrete rheology and monographs looking into prestressing. The paper is based on the existing fragments of the technical design documents concerning the bridges in question. The bridges were designed by Polish civil engineers.

Authors and Affiliations

S. Karaś

Theology Department of John Paul II Catholic Uniwersity of Lublin

Marta Lizut

Studia Nauk Teologicznych PAN | 2008 | Tom 3 | 169-180

Keywords John Paul II Catholic University of Lublin Theology Department theology scientific research

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Abstract

The Theology Department was opened in January 1918. It came into existence as one of the first four departments of the Catholic University of Lublin. Its activity became part of the university’s mission which is conducting research in harmony with science and faith, educating the catholic intelligentsia and contributing to christian culture.

The identity of the Department manifests itself in the high standard of scientific research and academic education as well as in deepening and promoting the christian concept of the world and man in the context of challenges of the present time.

This article presents an outline history, organization and the main trends in scientific research carried out in the Theology Department of John Paul II Catholic University of Lublin.

Authors and Affiliations

Marta Lizut

„Biuletyn Informacyjny” i „Biuletyn Informacyjny LKDS. Wydanie Strajkowe” — samoistne wydawnictwa periodyczne Lubelskiego Klubu Dziennikarzy Studenckich z 1981 r.

Barbara Centek

Rocznik Historii Prasy Polskiej | 2018 | t.21 | z.1

Keywords Polska Lublin PRL LKDS SZSP NZS studencki ruch dziennikarski studencki ruch wydawniczy czasopisma studenckie strajk studencki 1981 „Biuletyn Informacyjny” „Biuletyn Informacyjny LKDS. Wydanie Strajkowe”

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Abstract

Studencki strajk jesienią 1981 r. był czasem wzmożonej studenckiej aktywności kulturalnej. Powstawały wówczas inicjatywy wydawnicze niezależne od cenzury. W tych też okolicznościach studenci zrzeszeni wokół Lubelskiego Klubu Dziennikarzy Studenckich wznowili „Biuletyn” Informacyjny”, którego pełny tytuł tym razem brzmiał „Biuletyn Informacyjny LKDS. Wydanie Strajkowe”. Postrzegane jako organ SZSP czasopismo nie zawsze było akceptowane przez młodzież skupioną w NZS, a jednocześnie budziło podejrzenia wśród władz PRL.

Authors and Affiliations

Barbara Centek

1

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