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    Wyświetlanie 1-5 z 5
    Tytuł:
    Petrographic Garden in Moryń : a new geotouristic attraction in western Poland
    Autorzy:
    Górska-Zabielska, M.
    Dobracki, R.
    Powiązania:
    https://bibliotekanauki.pl/articles/294938.pdf
    Data publikacji:
    2015
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    erratic
    petrographic garden
    geodiversity
    geological heritage
    geotourism
    north-western Poland
    Opis:
    A new petrographic garden was established in 2012 in Moryń, north-western Poland. Thirty five erratics, derived from adjacent till moraines, witness local geological heritage and form a new geotouristic attraction. Together with other geovalues of this region, the petrographic garden is a cornerstone of the Polish-German geopark “Glacial Land over the Odra River” (Ger. Geopark Eiszeitland am Oderrand).
    Źródło:
    Landform Analysis; 2015, 29; 73-80
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The petrography of glacial sediments in Uckermark, NE Brandenburg : a preliminary study
    Autorzy:
    Górska, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/295004.pdf
    Data publikacji:
    2003
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    indicator erratic
    petrography
    Pommeranian phase
    last glacial
    Odra lobus
    Uckermark
    Brandenburg
    Opis:
    The Brandenburg section of the hinterland and of the maximum extent of the Pommeranian phase of the last glaciation, formed in two lobes (Schulz, 1967): Joachimsthal-Ringenwalder and Ucker-markischer, have been covered by a study on petrography of a gravelly and a stony fraction. The methods applied followed suggestions of Bose (1989), Trembaczowski (1961, 1967), Meyer (1983), Smed (1993, 1994) and Zandstra (1999). Petrographical analyses undertaken in Uckermark, NE Germany, were focused on: 1) observation of the dynamics of petrographical features along and in the hinterland of the Odra lobus on the German side, 2) indication of the western limit of the Odra lobus upon petrography of glacial sediments, 3) indication of Scandinavian parent areas of sediments of the Pommeranian phase and estimating the routes of ice-sheet onto German Lowland. The distance between outcrops of Scandinavian rocks causes the number of erratics in sediments of glacial accumulation in the German part of the Odra lobus. There are more Mesosoic rocks in the gravelly fraction as compared with sediments of the same age, but sampled in the Polish part of the Odra lobus. The stony fraction (20-60 mm) is represented mainly by indicator erratics from Smĺland and the Swedish coast in Kalmar Strait. Ĺland erratics, quite frequent in Polish lowlands, are observed rarely in Uckermark. Among statistical erratics there are numerous flints and Mesosoic limestones as well as Lower-Palaeozoic limestones. The theoretical stone centre moves its locality within middle-southern Smĺland.
    Źródło:
    Landform Analysis; 2003, 4; 39-48
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Early Piast dynasty (10–11th century) stone architecture in western Poland in a geological context
    Autorzy:
    Skoczylas, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060578.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    glacial erratic
    mortar
    quartzite sandstone
    gypsum
    limestone
    early Piast monumental architecture
    Opis:
    There is no consistency in reporting the stone material used to construct the first structures in the early Piast dominion (10–11th century) in Poland. The role and importance of the type of the stone building material used at that time has been underappreciated if not completely ignored. It has been stated that glacial erratics comprise the fundamental rock material used in the early Middle Ages for building, representing up to 98% of construction material. The remaining rocks used in building construction included local calcareous sinter, bog iron ores, Jurassic limestone from the Piechciny-Barcin region and gypsum from a salt dome in the village of Wapno in western Poland, while Miocene sandstone excavated at the inception of the Polish state in the Brzeźno Quarry near Konin has received significant attention. There appear to have been distinct phases of use of the various types of rock material. There was likely a link between the development of tillage and the development of monumental stone architecture from the Middle Ages. Deforestation resulting from the development of agriculture helped expose the glacial erratics used in the stone architecture of the first Piast rulers.
    Źródło:
    Geological Quarterly; 2017, 61, 4; 765--770
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Sexual dimorphism and pore systems in Ordovician ostracodes
    Autorzy:
    Schallreuter, R.E.L.
    Hinz-Schallreuter, I.C.U.
    Powiązania:
    https://bibliotekanauki.pl/articles/22627.pdf
    Data publikacji:
    2010
    Wydawca:
    Polska Akademia Nauk. Instytut Paleobiologii PAN
    Tematy:
    sexual dimorphism
    pore system
    paleontology
    Ordovician
    ostracod
    Arthropoda
    Crustacea
    Ostracoda
    Levisulculus
    Swantina
    Ampletochilina
    erratic boulder
    dimorphism
    adventral radial pore
    Baltoscandia
    Opis:
    Open antra, a special form of external brood pouches in Ordovician ostracodes suitable for both egg and brood care, are enabled by the associated pore system. Special kinds of radial pores connected with the adventral sculptures are described for the first time. Relationships exist between antral development and lifestyle in that open antra occur in nektobenthic taxa, while closed antra (false brood pouches) are connected with a benthic lifestyle. Taxa, particularly those with open antra, which are morphologically very similar in being non−lobate or non−sulcate, can be distinguished by the construction of the respective antra and the associated pore systems, as exemplified by Levisulculus, Swantina, and Ampletochitina.
    Źródło:
    Acta Palaeontologica Polonica; 2010, 55, 4
    0567-7920
    Pojawia się w:
    Acta Palaeontologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Exotic trilobites from the uppermost Cambrian Series 3 and lower Furongian of Sweden
    Autorzy:
    Żylińska, A.
    Weidner, T.
    Ahlgren, J.
    Ahlberg, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/139294.pdf
    Data publikacji:
    2015
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    Trilobita
    Cambrian Series 3
    Furongian
    Alum Shale
    glacial erratic boulders
    Sweden
    Denmark
    Scandinavia
    Exotic trilobites
    Trylobity
    trzeci oddział kambru
    Furong
    łupek ałunowy
    polodowcowe głazy narzutowe
    Szwecja
    Dania
    Skandynawia
    egzotyczne trylobity
    Opis:
    Seventeen taxa of exotic trilobites representing eight families are described from the olenid- and agnostoid-dominated strata of the uppermost Cambrian Series 3 and lower Furongian alum shale facies of Sweden and from glacial erratic boulders of Denmark. Only five taxa are assigned to species level, i.e., Maladioidella abdita (Salter, 1866), Olentella rara (Westergård, 1922), Pedinocephalus peregrinus (Henningsmoen, 1957), Ptychoparia pusilla (Westergård, 1922), and Westergaardella olenorum (Westergård, 1922), whereas the others are left under open nomenclature or remain unrecognized. Most are described for the first time from the Cambrian of Scandinavia. Their affinities point to a strong connection with East Gondwana, Laurentia, Kazakhstania and Siberia. Exotic trilobites appear in the succession directly after periods of very low oxygen concentration in the Alum Shale Sea; their occurrences correspond to the ranges of agnostoid arthropods in the succession and seem to be linked to global transgressive events causing an influx of cool and/or oxygen-depleted waters onto the shelf of the Baltica palaeocontinent.
    Źródło:
    Acta Geologica Polonica; 2015, 65, 1; 21-67
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-5 z 5

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