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Wyświetlanie 1-3 z 3
Tytuł:
Mikrofacje utworów węglanowo-silikoklastycznych miocenu w dolinie Opatówki (północna marginalna strefa zapadliska przedkarpackiego)
Microfacies of Miocene siliciclastic-carbonate deposits in the Opatówka Valley (northern marginal zone of the Carpathian Foredeep)
Autorzy:
Czarniecka, U.
Powiązania:
https://bibliotekanauki.pl/articles/2074883.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dolina Opatówki
zapadlisko przedkarpackie
utwory węglanowo-silikoklastyczne
formacja Pińczowa
formacja Chmielnika
petrografia
mikrofacje
Opatówka Valley
Carpathian Foredeep
siliciclastic-carbonate deposits
Pińczów Formation
Chmielnik Formation
petrography
microfacies
Opis:
The study concerns the Miocene carbonate and mixed siliciclastic-carbonate deposits of the Pińczów and Chmielnik Formations. They are located on the south-eastern slopes of the Holy Cross Mountains. Based on the thin sections analysis the framework components, kinds of cements and character of porosity were described. The framework components were qualified according to their size, roundness and sorting. Two types of components predominate: carbonate intraclasts and non-carbonate extraclasts. Among the intraclasts, mainly well rounded algal bioclasts occur. Moreover, poorly rounded skeletal elements of bryozoans, foraminifera, echinoids, serpulids, bivalves, gastropods, as well as rare glauconite grains have also been observed. The extraclasts are represented mainly by quartz grains and rare litoclasts, among which fragments of sandstones and limestones were recognized. These grains are poorly rounded or angular. Overall, the framework components are poorly sorted. Microspar is the main kind of pore-filling carbonate cements. The examined deposits have considerable porosity. The following types of porosity were distinguished: intergranular, intragranular, intercrystalline, moldic and vuggy. Based on the results of thin sections analysis, seven types of microfacies were distinguished: algal foraminiferal packstone, algal packstone, quartz-rich algal packstone, lithoclastic algal packstone, quartz-rich bryozoan algal packstone, bryozoan packstone, quartz-rich bryozoan packstone.
Źródło:
Przegląd Geologiczny; 2011, 59, 9; 625-632
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New data on the age of the sedimentary infill of the Orava-Nowy Targ Basin : a case study of the Bystry Stream succession (Middle/Upper Miocene, Western Carpathians)
Autorzy:
Wysocka, A.
Łoziński, M.
Śmigielski, M.
Czarniecka, U.
Bojanowski, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059754.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
tuffite
terrestrial facies
U-Pb geochronology
strike-slip faulting
Miocene
Orava-Nowy Targ Basin
Opis:
The Neogene sedimentary succession of the Orava-Nowy Targ Basin directly overlies the Central Carpathian Paleogene Basin deposits, the Magura Unit, and the Pieniny Klippen Belt. It provides an excellent geological record that postdates the main Mesoalpine structural and geomorphological processes in the Western Carpathians. Sedimentological, petrographical and geochronological investigations have allowed forthe re-examination of pyroclastic material, zircon dating, and a discussion on the relation of the Orava-Nowy Targ Basin to the exhumation of the Tatra Massif. The Bystry Stream succession is composed of NNW-inclined freshwater siltstones, sandstones and conglomerates. A few small, sometimes discontinuous, light grey intercalations of pyroclastic deposits and a single 1-2 m thick tuffite layer occur in the upper part of the succession. The tuffite contains an admixture of organic matter and siliciclastic grains (e.g., mica), suggesting that the volcanic ash fall was accompanied by normal deposition from weak currents. Sedimentation of deposits of the Bystry Stream succession took place in terrestrial settings, predominantly on floodplains and in rivers, in the vicinity of a hilly area supplying the basin with eroded material. The age of the tuffite layer from the Bystry Stream succession was determined at 11.87 +0.12/-0.24 Ma. The source of volcanogenic material in the tuffite was probably volcanic activity in the Inner Carpathians-Pannonian region, where effusive and volcanoclastic sillca-rich rocks were being produced by extrusive and explosive activity ~12 Ma. Obtained result connects the development of the Orava-Nowy Targ Basin at ~12 Ma with the late stage of the main episode of the Tatra Massif exhumation between ~22-10 Ma.
Źródło:
Geological Quarterly; 2018, 62, 2; 327--343
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New data on the continental deposits from the Cao Bang Basin (Cao Bang-Tien Yen Fault Zone, NE Vietnam) - biostratigraphy, provenance and faciespattern
Autorzy:
Wysocka, A.
Pha, D. P.
Durska, E.
Czarniecka, U.
Thang, D. V.
Filipek, A.
Cuong, N. Q.
Tuan, D. M.
Huyen, N. X.
Tha, H.V.
Powiązania:
https://bibliotekanauki.pl/articles/138599.pdf
Data publikacji:
2018
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
continental environments
pollen
spores
provenance
Palaeogene
Cao Bang
Vietnam
środowisko lądowe
pyłek
zarodniki
proweniencja
paleogen
Wietnam
Opis:
The Cao Bang Basin is the northernmost of the basins related to the Cao Bang-Tien Yen Fault Zone in northern Vietnam. The basin is filled with a thick series of continental deposits. However, the exact age of the sedimentary basin infill has been under discussion for a long time. Because of new published data, the authors have decided to revisit this basin. Palynological data has allowed us to assign the Cao Bang Basin infill to the Lower Oligocene PC1 complex of the Shangcun Fm. (southern China). Among the saccate grains of gymnosperms, the domination of Cathaya and Pinus was observed, whereas angiosperms are represented by Carya, Celtis, Hammamelidaceae, Ulmus and also Pterocarya, Quercus, the Castanea–Castanopsis–Lithocarpus group, and the Loranthaceae. Among pteridophytes occur Laevigatosporites, Osmundaceae, and Pteris. The sedimentological features of the Cao Bang Basin are distinct from those of other basins from the Cao Bang-Tien Yen Fault Zone. The basin is filled with a wide variety of clastic deposits, from some of coarse-grained, alluvial-fan origin, through sandy beds of fluvial origin up to fine, organic-rich lacustrine deposits. The coarse-grained lithofacies are built of clasts derived mainly from local sources. The sandstones from the basin equally are submature or immature. They contain a lot of lithoclasts, the composition of which depends on the sample location within the basin. The potential source area is composed of older sedimentary units and of granitic rocks. The geochemical samples studied reflect the geochemical composition of silicic source rocks with only a minor contribution of basic components. The succession that fills the basin is interpreted as a typical fill for relatively long-lasting evolving half-graben or strike-slip basins. Moreover, the basin is partly occupied by a subsequent present-day sedimentary basin of Quaternary age.
Źródło:
Acta Geologica Polonica; 2018, 68, 4; 689-709
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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