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Wyszukujesz frazę "Flysch belt" wg kryterium: Temat


Wyświetlanie 1-4 z 4
Tytuł:
Cretaceous (Aptian/Albian-?Cenomanian) age of “black flysch” and adjacent deposits of the Grajcarek thrust-sheets in the Male Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians)
Autorzy:
Oszczypko, N.
Olszewska, B.
Malata, E.
Powiązania:
https://bibliotekanauki.pl/articles/2059409.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
black flysch
Cretaceous
foraminifera
Pieniny Klippen Belt
Opis:
Several sections record the relation between the “black flysch” and Upper Cretaceous red shales in the Grajcarek thrust-sheets. In all the sections studied the “black flysch” appears in the core of imbricated folds or thrust-sheets, whereas the limbs are composed of Upper Cretaceous deposits. The transitional beds between the “ black flysch” and the Upper Cretaceous red shales are composed of green and black bituminous shales, green and red radiolarites and cherty limestones. Biostratigraphical investigations have revealed a similar type and sequence of microfauna assemblages in all the sections studied and significant redeposition of Jurassic calcareous benthic foraminifera, calcareous nannoplankton, molluscs, sponge spicules and crinoid elements. The Cretaceous age (Aptian/Albian-?Cenomanian) of the “black flysch” is shown by the presence of agglutinated foraminifera and microfacies data. These deposits are underlain by a Kimmeridgian-Aptian radiolarite/limestone condensed succession and overlain by Turonian-Campanian hemipelagic red shales and Maastrichtian/Lower Paleocene conglomerates and thick-bedded silicilastic turbidites of the Jarmuta Formation. Such a sequence of deposits is typical of the Outer Carpathian basins and records the global Mid/Late Cretaceous phenomena in the world ocean, followed by the Cretaceous Oceanic Red Beds.
Źródło:
Geological Quarterly; 2012, 56, 3; 411--440
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dinoflagellate cysts from the Szlachtowa Formation (Jurassic) and adjacent deposits (Jurassic–Cretaceous) of the Grajcarek Unit at Szczawnica-Zabaniszcze (Pieniny Klippen Belt, Carpathians, Poland)
Autorzy:
Gedl, P.
Powiązania:
https://bibliotekanauki.pl/articles/2060549.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Szlachtowa Formation
black flysch
biostratigraphy
Jurassic
Cretaceous
Pieniny Klippen Belt
Opis:
The Jurassic–Cretaceous fine-clastic dark deposits of the Grajcarek Unit (Pieniny Klippen Belt, Carpathians, Poland) show lithological similarities, which may lead to erroneous age correlations. Their well-exposed outcrop at Szczawnica-Zabaniszcze allows detailed sampling for their precise age determination. For this purpose, dinoflagellate cysts have been studied from a set of samples collected from the Szlachtowa, Opaleniec, Pieniny Limestone, Kapuśnica and Wronine formations exposed at that site (additional sample from the Pieniny Limestone Formation was studied). The Szlachtowa Formation, a very characteristic lithostratigraphic unit, which consists of black shale and sandstones extremely rich in mica flakes, occasionally referred to literature as the so-called "black flysch", yielded rich and well-preserved assemblages. Their age is Middle Jurassic, spanning the Aalenian to Lower Bajocian. The exposures of the Szlachtowa Formation at Szczawnica-Zabaniszcze are located close to the outcrops of the Opaleniec Formation. The calcareous spotted shale from this lithostratigraphic unit yielded rich dinoflagellate cyst assemblage characteristic for Late Bathonian (Early Callovian). The Opaleniec Formation tectonically contacts with very similar non-calcareous spotted shale of the Wronine Formation. Its age, based on infrequent dinoflagellate cysts is Aptian–Albian. Similar, Lower Aptian age was concluded for the Kapuśnica Formation. Late Barremian–earliest Aptian dinoflagellate cysts have been found in the underlying topmost part of the Pieniny Limestone Formation.
Źródło:
Geological Quarterly; 2013, 57, 3; 485--502
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Early to Late Bajocian age of the "black flysch" (Szlachtowa Fm.) deposits: implications for the history and geological structure of the Pieniny Klippen Belt, Carpathians
Autorzy:
Barski, M.
Matyja, B. A.
Segit, T.
Wierzbowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2059400.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Pieniny Klippen Belt
black flysch
stratigraphy
dinoflagellate cysts
palaeogeography
Magura Basin
Opis:
The "black flysch" deposits (Szlachtowa Formation at Podubocze near Czorsztyn in Poland), attributed so far to the Pieniny Klippen Basin successions, and at Hałuszowa in Poland as well as at Kamienka in Eastern Slovakia, attributed to the Grajcarek Succession of the Magura Basin, have yielded rich dinoflagellate cyst assemblages consisting of forms both redeposited (from Upper Triassic to Aalenian) and indigenous (Lower Bajocian to Upper Bajocian). An Early to Late Bajocian age of the deposits investigated is thus indicated, and this along with other stratigraphical, sedimentological and tectonic data indicates that all the deposits in question represent the early stages of development of the Magura Basin. The formation of “black flysch” deposits was possibly related to the Early Bajocian uplift of the Czorsztyn Ridge which resulted from the opening of the Magura Ocean. The occurrence of the deposits of the Magura Basin below the overthrusted deposits of the Klippen Basin (Czorsztyn Unit) in the area of study results in a marked change in the structural interpretation of the Pieniny Klippen Belt.
Źródło:
Geological Quarterly; 2012, 56, 3; 391-410
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wiek formacji szlachtowskiej (tzw. czarnego fliszu) i formacji z Opaleńca pienińskiego pasa skałkowego w Polsce na podstawie badań dinocyst
The age of the Szlachtowa Formation (the so-called "black flysch") and the Opaleniec Formation (Pieniny Klippen Belt, Poland) based on dinoflagellate cyst studies
Autorzy:
Gedl, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074578.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dinocysty
biostratygrafia
jura
formacja szlachtowska
formacja z Opaleńca
czarny flisz
Polska
dinoflagellate cysts
biostratigraphy
Jurassic
Szlachtowa Formation
Opaleniec Formation
black flysch
Pieniny Klippen Belt
Polska
Opis:
The Szlachtowa and the Opaleniec formations (Pieniny Klippen Belt, Poland) contain rich dinoflagellate cyst assemblages. The one from the Szlachtowa Formation (previously known as the "black flysch") is dominated by specimens representing the genera Dissiliodinium and Nannoceratopsis. The age of dinoflagellate cysts from this lithostratigraphic unit can be assumed as the Aalenian-Bajocian. Another assemblage occurs in the Opaleniec Formation. Being taxonomically more diverse, it contains several species including Ctenidodinium combazii, C. ornatum, Endoscrinium asymmetricum, Epiplosphaera gochtii, E. reticulata, Atopodinium prostatum, Adnatosphaeridium caulleryi. Age-range of this assemblage can be estimated as the Bajocian-Bathonian. No indications of Jurassic fossil redeposition that could justify suggestions of Cretaceous age of these lithostratigraphic units have been found.
Źródło:
Przegląd Geologiczny; 2008, 56, 3; 245-252
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-4 z 4

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