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Wyszukujesz frazę "Michniewicz, Jacek" wg kryterium: Autor


Wyświetlanie 1-3 z 3
Tytuł:
PROWENIENCJA SUROWCA RZEŹB I KOLUMN ZE STRZELNA Z KOLEKCJI MUZEUM NARODOWEGO W POZNANIU W ŚWIETLE BADAŃ PETROGRAFICZNYCH
ORIGIN OF THE RAW MATERIAL OF THE SCULPTURES AND COLUMNS FROM STRZELNO IN THE COLLECTIONS OF THE NATIONAL MUSEUM IN POZNAN IN THE LIGHT OF PETROGRAPHIC RESEARCH
Autorzy:
Michniewicz, Jacek
Powiązania:
https://bibliotekanauki.pl/articles/539544.pdf
Data publikacji:
2006
Wydawca:
Narodowy Instytut Dziedzictwa
Tematy:
NATIONAL MUSEUM IN POZNAN
PETROGRAPHIC RESEARCH (STRZELNO MONUMENTS)
SANDSTONE ORIGINS
Opis:
The research note discusses the outcome of petrographic studies relating to five Romanesque stone monuments from Strzelno, featured at the National Museum in Poznan. The research encompassed: - a perpendicular fragment of a column shaft 50 x 24 cm (dep. 64), originating from the post-Premonstratensian church of the Holy Trinity in Strzelno, covered with an ornamental tendril; - a fragment of the shaft of a column with an angel 28 x 28 x 28 cm (dep. 564) from the church of the Holy Trinity; - the head of Christ from the foundation tympanum in the rotunda of St. Prokop, damaged in a fire from 1945 (P. 19); - the head of a statue 22 x 20 x 21 cm (dep. 563), unearthed in the course of archaeological excavations in front of the rotunda of St. Prokop in 1950; - a column capital 40 x 36 x 20 cm (dep. 65) from the church of the Holy Trinity, with acanthus leafs in the corners and a fragment of a lamb. The examined monuments disclosed the presence of two types of sandstone: white quartzose sandstone, used for making the shaft of the column covered with an ornamental tendril, the shaft of a column with an angle, and the head of Christ, as well as subarkose sandstone used for the head of the statue and the column with acanthus leafs. It is difficult to propose an unambiguous origin of the white sandstone which could have been mined in the Warta river valley, e. g. near Konin-Brzezno (Tertiary sandstone), or in the Sudety Mts. in the regions of Zlotoryja, Lwowek Slaski, and Boleslawiec, as well as in Klodzko - between Polanica, Radkow and Krzeszowice (Cretaceous sandstone). The mineral composition of the red sandstones, their colour, and the presence of a calcite-clayey cement indicate a resemblance to the Permian period (Rotliegend) or Triassic sandstone (Buntsandstein) which do not occur in the Polish lowlands, and whose nearest outcroppings are located in the Sudety Mts. Particular attention is drawn to the petrographic similarity of this raw material to the sandstone in the portal of the abbey in Olbin, inserted into the southern nave of the church of St. Mary Magdalene in Wroclaw. The establishment of a connection between those monuments was rendered possible by a petrographic expert study of the abbey portal sandstone conducted by Alfred Majerowicz in 1963. The description contained therein corresponds to the petrography of the red sandstones from Strzelno. This similarity cannot be regarded as accidental since the raw material in question is not universally available. A sculptor could have used a similarly coloured raw material but he was unable to perceive the forms of the microscopic kaolinite crystals and the carbonates between the quartz grains. Consequently, we may conclude that the sandstone was brought over to Strzelno (in a raw form or as a completed work) probably by the same stone-cutters who made the portal for Olbin Abbey.
Źródło:
Ochrona Zabytków; 2006, 1; 91-102
0029-8247
Pojawia się w:
Ochrona Zabytków
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrographic Variability of the Fabrics of Wine Jars from Sha‘ar-Ha Amakim as a Reflection of Differences in Their Provenance and Chronology
Autorzy:
Michniewicz, Jacek
Młynarczyk, Jolanta
Powiązania:
https://bibliotekanauki.pl/articles/484083.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Kultur Śródziemnomorskich i Orientalnych PAN
Tematy:
Sha‘ar-Ha Amakim
wine jars
Persian period
Hellenistic period
Roman period
jars petrography
Opis:
The aim of the present study is to investigate the relationship between the shape of the Levantine wine jars discovered at Sha‘ar-Ha Amakim and the petrography of their respective fabrics. The majority of sampled ceramic material originates in well-defined chronological phases of the settlement at the site, spanning the Persian through to the Middle Roman periods. The obtained results clearly demonstrate a connection between the historical period and the raw materials used in jar production. Specifically, the jars of the Phoenician type used in the Persian and Hellenistic periods were made from a fairly homogeneous raw material, the features of which such as the content of the fragments of the coralline alga Amphiroa confirm the previous results of the investigations of jars whose fabric has been considered as Phoenician. On the other hand the bag-shaped jars, especially those of the Hellenistic period, are characterized by the more diversified petrography of their fabrics, suggesting that they were produced by a number of local workshops to supply the needs of local wineries. Finally, the Roman period brings an abrupt change in the production of wine containers, with the introduction of the common use of the fine ferruginous soil rich in quartz silt.
Źródło:
Études et Travaux (Institut des Cultures Méditerranéennes et Orientales de l’Académie Polonaise des Sciences); 2017, 30; 339-387
2084-6762
2449-9579
Pojawia się w:
Études et Travaux (Institut des Cultures Méditerranéennes et Orientales de l’Académie Polonaise des Sciences)
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Manganese pebbles from Hochschartehöhlesystem (the Hoher Göll Massif, Austria): insight into potential genesis and provenance
Autorzy:
Kicińska, Ditta
Michniewicz, Jacek
Kubiak, Michał
Powiązania:
https://bibliotekanauki.pl/articles/24201053.pdf
Data publikacji:
2023
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Northern Calcareous Alps
cave sediments
manganese pebbles
submarine vents
braunite
Opis:
Heavy, black manganese pebbles have been found in the clastic sediments of the Hochschartehöhlensystem (the Northern Calcareous Alps). Six selected pebbles were subjected to X-ray diffraction, optical microscopy and optical and electron microscopy analysis. The results reveal that the main component of the pebbles is manganese silicate, braunite, Mn2+Mn3+6(SiO4)O8. Braunite is a mineral formed at elevated temperatures, mainly through hydrothermal, metamorphic or diagenetic processes. This means that the manganese pebbles were formed outside the caves. However, manganese rock was not found in situ on the surface of the Hoher Göll Massif. This probably indicates that their origin is from eroded parts of Mesozoic rocks. The first studies of pebbles and their mineralogy, by analogy with contemporary marine sediments, indicate that their genesis is related to spreading zones and accompanies hydrothermal vents. The analysed material highlights two important issues: (1) the manganese pebbles are significant arguments for the occurrence of hydrothermal vents in the Northern Calcareous Alps; and (2) the importance of cave sediments studies, which provide relevant evidence for palaeogeographic reconstruction.
Źródło:
Annales Societatis Geologorum Poloniae; 2023, 93, 2; 211--223
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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