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Wyświetlanie 1-3 z 3
Tytuł:
Depositional conditions of the Upper Younger Loess during the Last Glacial Maximum in central and eastern Europe
Autorzy:
Dzierżek, Jan
Lindner, Leszek
Chlebowski, Roman
Szymanek, Marcin
Bogucki, Andriy
Tomeniuk, Olena
Powiązania:
https://bibliotekanauki.pl/articles/24024703.pdf
Data publikacji:
2022
Wydawca:
Polska Akademia Nauk. Czasopisma i Monografie PAN
Tematy:
North European Loess Belt
Vistulian glaciation
aeolian processes
palaeowind circulation
heavy minerals
północnoeuropejski pas lessowy
zlodowacenie Wisły
procesy eoliczne
minerały ciężkie
Opis:
This paper is a summary of the results of research on the accumulation conditions of the Upper Younger Loess (LMg) in Poland and Bug loess (bg) in Ukraine from the maximum stage (MIS 2) of the Vistulian (Weichselian) Glaciation in central and eastern Europe. These studies included an analysis of the morphological (topographic) situation of the loess cover, its grain size and heavy mineral composition, the preserved structures of loess sedimentation as well as mollusc and pollen analyses of this loess. They revealed that the accumulation of Upper Younger Loess (UYL) might have been more dependent on the prevailing moisture conditions than previously thought. These conditions could have been caused by cold air masses from an ice sheet and warm air masses from the Mediterranean Sea and Atlantic coming together in the Carpathians and the Holy Cross Mountains and favouring the formation of dust storms and precipitation. In this process, a loading of loess dust (formed from local rocks weathering in periglacial conditions) by atmospheric moisture particles was especially significant. The moist substrate not only favoured the periodic development of vegetation and molluscs but also enabled the interception of dust and the accumulation of an increasingly thick loess cover. Westerly and south-westerly winds predominated in the UYL as indicated by the topographic position of loess patches and the mineral composition of the studied loess. Periodically an increased air circulation from the east and northeast occurred.
Źródło:
Acta Geologica Polonica; 2022, 72, 4; 369--389
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New data on the age and stratigraphic relationships of the Czajakowa Radiolarite Formation in the Pieniny Klippen Belt (Carpathians) based on the radiolarian biostratigraphy in the stratotype section
Autorzy:
Bąk, M.
Chodacka, S.
Bąk, K.
Okoński, S.
Powiązania:
https://bibliotekanauki.pl/articles/139119.pdf
Data publikacji:
2018
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Middle-Late Jurassic
radiolaria
taxonomy
biostratigraphy
Czajakowa Radiolarite Formation
pelagic siliceous facies
Pieniny Klippen Belt
Carpathians
jura
promienica
taksonomia
biostratygrafia
Czajakowa Skała
radiolaryty z Czajakowej
Pieniński Pas Skałkowy
Karpaty
Opis:
The radiolarian biostratigraphy of the Middle–Upper Jurassic pelagic siliceous sediments (Czajakowa Radiolarite Formation) in the Niedzica succession of the Pieniny Klippen Belt (Carpathians) is interpreted in terms of their age in a stratotype section, and facies equivalents in other tectonic-facies units of this region. The siliceous sediments are represented by radiolarian cherts and silicified limestones which are underlain and overlain by red nodular limestones, equivalents of the Rosso Ammonitico facies. The radiolarian association includes thirty-seven taxa belonging to twenty one genera which represent the Northern Tethyan Palaeogeographic Province. Key radiolarians recorded provide a means of correlation with zonation schemes based on Unitary Associations defined for the Jurassic Tethyan sediments. The age of the Czajakowa Radiolarite Formation in the stratotype section is determined as U.A.Z.9 to U.A.Z.11 corresponding to middle Oxfordian up to Kimmeridgian. Comparison of radiolarian biozones from the stratotype section with other facial equivalent sections in the Pieniny Klippen Belt reveals a significant diachronism for both the lower and the upper limits of the Jurassic pelagic siliceous facies.
Źródło:
Acta Geologica Polonica; 2018, 68, 1; 1-20
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The new Northern Copper Belt of south-western Poland: a summary
Autorzy:
Speczik, Stanisław
Szamałek, Krzysztof
Wierchowiec, Jan
Zieliński, Krzysztof
Pietrzela, Alicja
Bieńko, Tomasz
Powiązania:
https://bibliotekanauki.pl/articles/24024700.pdf
Data publikacji:
2022
Wydawca:
Polska Akademia Nauk. Czasopisma i Monografie PAN
Tematy:
deep copper and silver deposits
Northern Copper Belt
Fore-Sudetic monocline
stratiform copper mineralization
Kupferschiefer -type deposits
głębokie złoża miedzi i srebra
północny pas miedziowy
monoklina przedsudecka
mineralizacja miedzi
łupek miedzionośny
złoża
Opis:
The Northern Copper Belt is located in south-western Poland, a region well known for its copper and silver occurrences of varying significance. This area also includes the abandoned mines of the North-Sudetic Trough (Old Copper District), as well as the currently active New Copper District in the southern part of the Fore - Sudetic Monocline. The vast exploration programme of Miedzi Copper Corp. initiated in 2011 in the northern, deeper part of the Fore Sudetic Monocline provided new data about the deeper parts of this geological unit, located north of the known deposits. A number of prospective areas with Cu-Ag mineralization were investigated, which ultimately resulted in the discovery of three new Cu-Ag deposits. Both the prospective areas and the documented deposits form the so-called Northern Copper Belt, which as a whole has high potential for the identification of new ore deposits and an increase in resources. A description of these three new deposits is provided along with characteristics of the areas of their possible extension, and the additional prospective areas with hypothetical and speculative resources. The new deposits are compared to other Polish Cu-Ag ore deposits, with an emphasis on differences in their geological structure and mineralogy. The paper also presents a brief summary of the applied new exploration tools which have led to this discovery.
Źródło:
Acta Geologica Polonica; 2022, 72, 4; 469--477
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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