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    Wyświetlanie 1-12 z 12
    Tytuł:
    Natural Evolution of Western Shore of a Sambian Peninsula on Completion of Dumping from an Amber Mining Plant
    Autorzy:
    Burnashov, E.
    Chubarenko, B.
    Stont, Z.
    Powiązania:
    https://bibliotekanauki.pl/articles/241446.pdf
    Data publikacji:
    2010
    Wydawca:
    Polska Akademia Nauk. Instytut Budownictwa Wodnego PAN
    Tematy:
    dumping
    South-East Baltic Sea
    Kaliningrad Amber Mining Plant
    Opis:
    This article shows how dumping of sediments from an amber mining plant prevented erosion of the western shore of the Sambian Peninsula (in Kaliningrad Oblast). The average annual dynamics of coastal areas in the vicinity of the former dumping site of the amber mining plant is described. Nowadays the erosion is continuing after cessation of dumping. The rate of erosion was estimated by results of regular monitoring measurements, using airborne laser scanning. It was found that about 250000 cubic metres per year of local material is needed every year to prevent further erosion and retreat of the shore.
    Źródło:
    Archives of Hydro-Engineering and Environmental Mechanics; 2010, 57, 2; 105-117
    1231-3726
    Pojawia się w:
    Archives of Hydro-Engineering and Environmental Mechanics
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Textile-impressed Pottery Revisited: Its Usefulness for Studying Bronze Age Textile Craft in Estonia
    Autorzy:
    Rammo, Riina
    Powiązania:
    https://bibliotekanauki.pl/articles/1774817.pdf
    Data publikacji:
    2019-01-10
    Wydawca:
    Uniwersytet Warszawski. Wydawnictwa Uniwersytetu Warszawskiego
    Tematy:
    textile impressions on ceramics
    textile ceramics
    Bronze Age
    textile technology
    East Baltic
    Opis:
    Although textile craft is a socially complex and economically significant phenomenon, little is known about textile techniques in the Bronze Age of the eastern shore of the Baltic Sea, including Estonia. No textile or cloth remains dated to the Bronze Age, i.e. between 1800 and 500 BC in the Estonian context, have been found so far. Only indirect evidence such as possible textile tools and impressions on pottery can be used in the study of textile-making. The aim of the present study is to review the available evidence regarding Bronze Age pottery with patterns commonly described as made with textiles, and to systematise it. As a result, it is suggested that the evidence based on these impressions is even more limited than thought so far. Few finds clearly indicate the use of textiles. Regular patterns consisting of variously-shaped concavities on the vessels’ walls may have been made also with other items, for example by rolling fir cones over the surface of a freshly-modelled pot.
    Źródło:
    Światowit; 2017, 56(1); 111-118
    0082-044X
    Pojawia się w:
    Światowit
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Apparatus of the conodont Scolopodus striatus Pander, 1856 and re-evaluation of Panders species of Scolopodus
    Autorzy:
    Tolmacheva, T Y
    Powiązania:
    https://bibliotekanauki.pl/articles/20625.pdf
    Data publikacji:
    2006
    Wydawca:
    Polska Akademia Nauk. Instytut Paleobiologii PAN
    Tematy:
    apparatus
    Conodonta
    Scolopodus striatus
    East Baltic
    Russia
    Ordovician
    conodont
    morphotype
    paleontology
    Estonia
    identification
    Opis:
    The Lower Ordovician conodont Scolopodus striatus Pander, 1856 (= Scolopodus rex Lindström, 1955) has an apparatus composed of five element morphotypes: acontiodiform, subrounded, compressed paltodiform, paltodiform, and scandodiform. The identification of the morphotypes is based on the general asymmetry of elements and shape of their bases. The elements are variable within each morphological group and form a continuous transition series generally reflected in differences in the depth of the basal cavity, height and degree of lateral compression of the base. The new collection from the localities near St. Petersburg, the type area of the first investigations on conodonts by Christian Pander in 1856, was examined and species of Scolopodus named by him are revised. All Pander’s species with the exception of the type species Scolopodus sublaevis are identified as a single species of Scolopodus that was named 99 years later as Scolopodus rex. The S. sublaevis sensu formae was not recognised in collections studied and its validity is questionable. S. striatus is the most easily recognisable among Pander’s species of Scolopodus and is here proposed to be a senior synonym of S. rex.
    Źródło:
    Acta Palaeontologica Polonica; 2006, 51, 2
    0567-7920
    Pojawia się w:
    Acta Palaeontologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Paleozoic rocks structure versus Cenozoic cuesta relief along the Baltic Shield–East European Platform transect
    Autorzy:
    Tuuling, I.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060390.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Baltic Homocline
    intracratonic forced folds
    Estonia
    Swedish east coast
    Cenozoic cuesta relief
    Baltic Klint
    Opis:
    Based on structural maps, the bedrock structure on the southern slope of the Baltic Shield is analysed. Gently southerly dipping (0.1–0.2°) Paleozoic layers from Estonia to the Swedish east coast form the Baltic Homocline (BH). Numerous monoclinal folds, forced by basement faulting, induce slight variations in bedrock attitude across the BH. Studies on faults exposed in Southern Finland suggest that many monoclinal folds inducing basement faults within the BH are of Precambrian origin and have been active in pulses. The present monoclines were shaped by the Caledonian Orogeny. Submeridional tectonic hinge-lines induce minor regional-scale changes in the structural setting and control trends/styles of the forced folds. From the west, the BH bounds with the Baltic–Bothnian mobile zone that has been intermittently active since Mesoproterozoic times. The evolving Baltic Syneclise in the Silurian rearranged the structural setting typical for the Ordovician Baltic Basin. The Cenozoic uplift of Scandinavia created a SE-to-E-dipping bedrock sequence around the Gotland–Öland area. As the latter area had a different attitude than the BH, two Cenozoic cuesta-sets started to evolve around the northern Baltic Proper. They both had an outlet to the N–S-flowing Eridanos River around the Gotska Sandön area, creating thus two independent sections of the Baltic Klint.
    Źródło:
    Geological Quarterly; 2017, 61, 2; 396--412
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Seismo-geological model of the Baltic Basin (Poland)
    Autorzy:
    Kasperska, Monika
    Marzec, Paweł
    Pietsch, Kaja
    Golonka, Jan
    Powiązania:
    https://bibliotekanauki.pl/articles/191810.pdf
    Data publikacji:
    2019
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Baltic Basin
    East European Platform
    Palaeozoic
    lithostratigraphy
    tectonics
    seismic interpretation
    Opis:
    The aim of this study is to construct a seismo-geological model of the western part of the Baltic Syneclise. This model enables reconstruction of the tectonic processes taking place in this area, which had a significant impact on the formation of prospective zones for the occurrence of unconventional hydrocarbon accumulations. The two seismic surveys Opalino 3D and Kościerzyna-Gdańsk 2D, together with borehole data available in the vicinity, were used for the research. Well data were used not only for the seismic-to-well tie, but also for the construction of well cross-sections (including balanced ones). The structural interpretation of seismic boundaries enabled the separation of four structural stages: Precambrian; Caledonian, Permian-Mesozoic and Cenozoic. The seismic interpretation of the Opalino 3D survey indicates the presence of block-style tectonics in this area. This system is considered to be a part of a large block system, also extending throughout the area of the 2D survey. The Caledonian interval shows the greatest degree of structural complexity. Most of the large Palaeozoic dislocations already had been formed in the Cambrian. They underwent reactivation and/or inversion in the Silurian, or in the final stages of the Caledonian and/or Variscan Orogeny, at the latest. The current shape and structure of the Baltic Syneclise and the development of the Palaeozoic sedimentary cover were significantly influenced by the processes taking place in the Teisseyre-Tornquist Zone (TTZ). The dislocations of the Lower Palaeozoic stage are characterized by general NW-SE and NE-SW trends, although the first of these seems to be dominant.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2019, 89, 2; 195-213
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Geological section through the lower Paleozoic strata of the Polish part of the Baltic region
    Autorzy:
    Pokorski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059065.pdf
    Data publikacji:
    2010
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Lower Paleozoic
    Baltic Region
    East European Craton
    West European Platform
    faults and fault zones
    structural elements
    Opis:
    The present-day structural pattern of the Baltic Depression developed due to superimposition of three main deformation phases: syn-Caledonian (after the Silurian), syn-Variscan (at the end of Carboniferous and beginning of Permian) and syn-Alpine (latest Mesozoic or earliest Cenozoic). The major restructuring of the area occurred as a result of syn-Variscan deformation that took place in latest Carboniferous and earliest Permian times. Most of the faults developed or became reactivated probably at that time. Syn-Alpine deformation manifested itself relatively weakly, mainly by reactivation of some pre-existing faults.
    Źródło:
    Geological Quarterly; 2010, 54, 2; 123-130
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Structure and development of the Valmiera-Lokno Uplift – a highly elevated basement block with a strongly deformed and eroded platform cover in the East European Craton interior around the Estonian-Latvian-Russian borderland
    Autorzy:
    Tuuling, I.
    Vaher, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060409.pdf
    Data publikacji:
    2018
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    East European Craton interior
    Baltic Homocline-Baltic Syneclise junction
    Liepaja-Riga-Pskov Fault Zone
    Valmiera-Lokno Uplift
    platform cover basement-cored anticlines
    strike-slip movements
    Opis:
    Based on drillings, a number of geological cross-sections, and structure contour and isopach maps were composed to describe/analyse the structure and development of the Valmiera-Lokno Uplift (VLU), a basement block elevated up to 700 m with a heavily deformed and eroded platform cover in the East European Craton interior, along the regional Liepaja-Riga-Pskov Fault Zone (LRPFZ). Five isolated basement-cored anticlines (BCA), the Lokno, Haanja, Mõniste, Valmiera and Smiltene uplifts, arise in the platform cover on the VLU, whereas the downthrown LRPFZ side defines a complex monoclinal fold. The anticlines, straddling or occurring near the monocline, merge with it and thus have highly asymmetrical shapes. Thickness changes of stratigraphic units across the VLU reveal its complex history, reflecting regional tectonic activation pulses that varied noticeably even between neighbouring BCAs. In all, the latest Precambrian-earliest Ordovician initiation epoch of the VLU was followed by modest tectonic activity or a standstill period in the Middle Ordovician-Early Silurian. Intensifying tectonic movements culminated again in the prime of the Caledonian Orogeny in latest Silurian-earliest Devonian time, and faded thereafter towards the end of Early Devonian. The VLU has been reactivated occasionally since the latest Devonian and emerges as a crustal weakness in the recent movement and seismicity patterns. To decipher the origin of the VLU, hitherto factually undiscussed topics, a more detailed study of the LRPFZ, analysis of its fault pattern and kinematics alongside the regional tectonic setting/history is needed. A cursory look hints to a substantial Early Paleozoic sinistral strike-slip along the LRPFZ, allowing interpreting the VLU as a possible restraining bend structure.
    Źródło:
    Geological Quarterly; 2018, 62, 3; 579--596
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Osiedla nawodne kultury kurhanów zachodniobałtyjskich w krajobrazie naturalnym i kontekście kulturowym północno-wschodniej Polski
    Lake settlements of the West Baltic Barrow culture in natural and cultural landscape of North-Eastern Poland
    Autorzy:
    Gackowski, Jacek
    Powiązania:
    https://bibliotekanauki.pl/articles/1365920.pdf
    Data publikacji:
    2017
    Wydawca:
    Instytut Północny im. Wojciecha Kętrzyńskiego w Olsztynie
    Tematy:
    Osiedla nawodne
    kultura kurhanów zachodniobałtyjskich
    wczesna
    epoka żelaza
    Polska północno-wschodnia
    Lake dwellings
    West Baltic Barrow Culture
    Early Iron Age
    North-East
    Polska
    Opis:
    This paper deals with the problem referred to the Early Iron Age lake settlement of the West Baltic Barrow culture and the cultural factors that affected the stilt houses among the local settlement patterns. This concept is based on the results achieved thus far for the lake settlements with a special emphasis on the sites in Mołtajny near Kętrzyn and Pieczarki near Giżycko (investigated during 1986-1992). The sites have provided the data concerning both the cultural and natural environment impact on the stilt housing Here it appears that the residents of such objects did not significantly differ from the communities that had inhabited neither fortified nor open settlements as it is reinforced by the same approach to farming and breeding strategies and similar manufacturing activities such as the bronze metalworking. Therefore the problem concerning the motives that led some groups of the West Baltic Barrow culture community to stilt housing remains still unresolved
    Źródło:
    Komunikaty Mazursko-Warmińskie; 2017, 295, 1; 3-22
    0023-3196
    2719-8979
    Pojawia się w:
    Komunikaty Mazursko-Warmińskie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Proterozoiczne podłoże krystaliczne polskiej części Bałtyku w świetle badań strukturalnych
    Astructural study of the Precambrian crystalline basement in the Polish sector of the Baltic Sea
    Autorzy:
    Cymerman, Z.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075274.pdf
    Data publikacji:
    2015
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    skały krystaliczne
    struktury tektoniczne
    odwierty
    Danopolonian orogenezy
    kraton wschodnioeuropejski
    południowy Bałtyk
    crystalline rocks
    tectonic structures
    boreholes
    Danopolonian orogeny
    East European Craton
    southern Baltic Sea
    Opis:
    This paper presents structural data and regional correlations based on drill cores from 8 boreholes (B2-1/80, B3-1/81, B4-1/81, B6-1/82, B6-2/85, B7-1/91, B16-1/85 and B21-1/95) penetrating Precambrian crystalline rocks in the Polish part of the Baltic Sea. The crystalline rocks from the ftom these boreholes were compared to cores from several wells in Eastern Pomerania, and the Kashubian and Warmia regions and above all with the Mesoproterozoic granitoids and metamorphic rocks of Bornholm and Southern Sweden. The pre-existing basement map of the Southern Baltic, showing Palaeoproterozoic or even Archaean granitoid massifs and narrow north-south fold belts is questioned. Instead, in the present interpretation, the studied area of the Polish part of the Southern Baltic Sea is underlain by a fragment of the Mesoproterozoic (ca. 1.47–1.43 Ga) Danopolonian („Hallandian”) orogeny, comprising mainly regional-scale ductile shear zones, which, striking probably in W–E to WNW–ESE directions, are characterized by the predominance of a thrust to transpressional strain regime with tectonic transport top-to-the S or SSW. The structural kinematic and lithological interpretations of these shear zones are based on comparison with the other parts of the East European Craton that are exposed in Bornholm and the Blekinge and Skne regions in Southern Sweden.
    Źródło:
    Przegląd Geologiczny; 2015, 63, 4; 228--238
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Angielska Kompania Wschodnia w handlu bałtyckim
    The Eastland Company in the Baltic Trade
    Autorzy:
    Groth, Andrzej
    Powiązania:
    https://bibliotekanauki.pl/articles/1602051.pdf
    Data publikacji:
    2015
    Wydawca:
    Uniwersytet Szczeciński. Wydawnictwo Naukowe Uniwersytetu Szczecińskiego
    Tematy:
    English Baltic trade
    the Eastland Company (North Sea Company/the Company of Merchants of the East)
    modern times
    angielski handel bałtycki
    Kompania Wschodnia
    czasy nowożytne
    Opis:
    Od XV stulecia stosunki handlowe Anglików z ziemiami nadbałtyckimi przybrały na sile i znaczeniu. Rynek bałtycki był ważnym odbiorcą angielskiego sukna, a jednocześnie zaopatrywał stocznie angielskie we wszystkie podstawowe surowce i półfabrykaty. Warto przypomnieć, że w drugiej połowie XVI w. surowce dla przemysłu okrętowego stanowiły od 1/2 do 3/4 angielskiego importu bałtyckiego, a wyroby tekstylne ponad 80% wartości angielskiego wywozu do krajów nadbałtyckich. Większość tych surowców była dostarczana przez gospodarkę państwa polsko-litewskiego, które do drugiej połowy XVII w. zachowało dominującą pozycję w wymianie handlowej Bałtyku z Zachodem. W bałtyckim handlu angielskim dominowały trzy porty: Elbląg, Gdańsk i Królewiec. Wiodąca pozycja Elbląga wynikała z faktu usytuowania w tym mieście angielskiej Kompanii Wschodniej. Po zawarciu rozejmu w Altmarku (1629 r.) Kompania Wschodnia znalazła się praktycznie bez rezydencji, gdyż jej pobyt w Elblągu stał się bezcelowy ze względu na ograniczenia nałożone przez Sejm Rzeczypospolitej na handel z portami znajdującymi się w rękach szwedzkich. Po likwidacji kantoru Kompanii Wschodniej w Elblągu bałtycki handel elbląski przejął Gdańsk, Królewiec i częściowo porty inflanckie. Od lat 80. XVII w. główny ciężar tego handlu przesunął się na porty szwedzkie. Angielski handel bałtycki odbywał się głównie za pośrednictwem portów wybrzeża wschodniego: Londynu, Hull i Newcastle.
    In the 15th century the economic relations between England and the Baltic countries became more intensified. The Baltic market was an important receiver of English cloth, and – at the same time – supplied the English shipyards with all the basic raw materials and semi-finished products. It is worth reminding that in the mid-16th century raw materials for the shipbuilding industry accounted for 1/2 to 3/4 of the Baltic exports to England, and textile products accounted for 80% of the value of the English imports to the Baltic countries. Most of these raw materials were delivered by the economy of the Polish-Lithuanian state, which up to the middle of the 17th century kept the dominant position in the commercial exchange between the Baltic region and the West of Europe. The key role in the Baltic trade with England was played by three ports: Elbląg (Elbing), Gdańsk (Danzig) and Królewiec (Königsberg). The prominent role of Elbląg resulted from the fact that the Eastland Company had its headquarters there. After the truce in Altmark was signed (1629) the Eastland Company practically lost its headquarters as its stay in Elbląg became pointless because of the restrictions imposed by the Polish Sejm (Parliament) on the trade with the ports under the Swedish rule. After the liquidation of the Eastland Company’s office in Elbląg the port’s participation in the Baltic trade was taken over by Gdańsk, Królewiec and partly by the Livonian ports. Since the 1680s the Baltic trade concentrated in the Swedish ports. In England the ports that participated in the Baltic trade were mainly the ones from the Eastern coast: London, Hull and Newcastle.
    Źródło:
    Studia Maritima; 2015, 28; 5-18
    0137-3587
    2353-303X
    Pojawia się w:
    Studia Maritima
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Litwa w systemie transportowym Regionu Morza Bałtyckiego
    Lithuania in the transport system of the Baltic Sea Region
    Autorzy:
    Ginc, Ernest
    Powiązania:
    https://bibliotekanauki.pl/articles/596831.pdf
    Data publikacji:
    2015
    Wydawca:
    Łódzkie Towarzystwo Naukowe
    Tematy:
    Region Morza Bałtyckiego (RMB)
    transport
    Korytarz Transportowy Wschód –
    – Zachód
    Kolej Bałtycka – Korytarz Wzrostu
    Baltic Sea Region (BSR)
    East–West Transport Corridor
    Rail Baltica Growth Corridor
    Opis:
    Region Morza Bałtyckiego na tle innych obszarów Europy można określić jako region stabilny gospodarczo i społecznie, o wysokiej aktywności inwestycyjnej podmiotów krajowych i zagranicznych. Niemniej, trudno jest mówić o RMB jako jednolitym obszarze gospodarczym. Podejmowane są liczne działania w ramach programu RMB, wśród których na uwagę zasługuje obszar dotyczący transportu. Litwa jako jeden z 11 krajów także uczestniczy w realizacji jednego z ważnych celów programu dotyczącego lepszego połączenia drugorzędnych i trzeciorzędnych sieci i węzłów w Regionie Morza Bałtyckiego z głównymi sieciami transportowymi zdefiniowanymi przez Partnerstwo TEN-T i Wymiaru Północnego w zakresie transportu i logistyki.
    The Baltic Sea Region, when compared to other parts of Europe, can be defined as an economically and socially stable region, with high investment activity of domestic and foreign entities. However, it is difficult to talk about the region as a homogeneous economic area. There are various activities undertaken within the Baltic Sea Region scheme, among which the transport area deserves particular attention. Lithuania as one of the 11 countries also participates in the implementation of one of the important objectives of the program. As a member of the BSR Lithuania aims at better connecting the secondary and tertiary transport networks and nodes in the Baltic Sea Region to core transport networks defined by the Partnership of the TEN-T and the Northern Dimension.
    Źródło:
    Studia Prawno-Ekonomiczne; 2015, XCVI (96); 223-238
    0081-6841
    Pojawia się w:
    Studia Prawno-Ekonomiczne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Balkan/Sydosteuropa och Östersjöregionen – en jämförelse
    Autorzy:
    Gustavsson, Sven
    Powiązania:
    https://bibliotekanauki.pl/articles/1177317.pdf
    Data publikacji:
    2011-01-01
    Wydawca:
    Uniwersytet im. Adama Mickiewicza w Poznaniu
    Tematy:
    Östersjöregionen och Sydosteuropa/Balkan Centraleuropa vs Europas periferi
    kulturgränser
    kulturzoner
    kulturell
    etnisk och språklig mångfald
    baltic sea region and south east europe/the balkans central europe vs. the periphery of europe
    Źródło:
    Folia Scandinavica Posnaniensia; 2011, 12; 91-102
    1230-4786
    2299-6885
    Pojawia się w:
    Folia Scandinavica Posnaniensia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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