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Wyświetlanie 1-2 z 2
Tytuł:
The Cenomanian heterozoan carbonates in the north-central Alborz, north-east Kelardasht, north Iran
Autorzy:
Kavoosi, Mohammad Ali
Ezoji, Neda
Powiązania:
https://bibliotekanauki.pl/articles/2060116.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
heterozoan carbonates
condensed
Cenomanian
north-east Kelardasht
Opis:
Detailed field surveys, petrographic investigation and SEM and EDS analyses have been used to evaluate Cenomanian glauconitic heterozoan carbonates in north-east Kelardasht, north-central Alborz, north Iran. Lithofacies and microfacies analyses led to recognition of six microfacies types related to the inner-, mid- and outer-ramp facies belts of a carbonate ramp. The heterozoan nature of these carbonates is inferred from a predominance of echinoderms associated with calcispheres, planktonic foraminifers, a lack of ooid grains, and a low carbonate production rate, together with a high content of glauconite grains and prevailing high-Mg calcite mineralogy. Petrographic and SEM studies reveal that glauconite filling skeletal grains retains the shape and morphology of host grains, signifying an authigenic origin at low sedimentation rates and slightly reducing conditions. SEM images show cauliflower and rosette structures associated with well-developed lamellae indicating an authigenic origin of evolved glauconite grains. Our findings are compatible with a nutrient-rich waters and palaeoecological stress related to relative sea-level rise and eutrophic conditions, which contributed to the generation of these heterozoan carbonates despite the hot greenhouse conditions during the Cenomanian in the north-central Alborz Mountains.
Źródło:
Geological Quarterly; 2021, 65, 3; 65: 37
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Facies variability in the Cambrian deposits from the Kościerzyna and Gdańsk sections (Pomeranian Caledonides foreland, northern Poland) : a comparative study
Autorzy:
Jaworowski, K.
Powiązania:
https://bibliotekanauki.pl/articles/2059452.pdf
Data publikacji:
2000
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
northern Poland
Cambrian
transgressive-regressive cycle
condensed deposit
sources of clastics
Opis:
The origin of Cambrian clastics occurring in the marginal part of the East European Craton, in the foreland of the Pomeranian Caledonides is discussed. They were deposited in an epicontinental sea influenced by tides and storms. The first Lower Palaeozoic transgressive-regressive (T-R) cycle spans the Lower and most of the Middle Cambrian. The maximum transgression in the craton-margin part (Kościerzyna section) is marked by submarine erosion and a very low deposition rate around the Lower/Middle Cambrian boundary. The condensed deposit is a limestone - shell hash packstone with phosphatized mudstone clasts. In the inner part of the craton (Gdańsk section), the condensed deposit is represented by mudstones and heterolithic deposits with iron ooids. Transgressive phase deposits of the first T-R cycle from the Kościerzyna section are 323.5 m thick, while regressive phase deposits - 273.7 m thick. In the Gdańsk section the thicknesses are of 113.0 and 218.8 m, respectively. Deposits of the first T-R cycle of northern Poland and the Polish part of the Baltic Sea are overlain by those of the second T-R cycle, which, when complete, comprise the uppermost Middle Cambrian, Upper Cambrian and Lower Tremadoc. In both the sections discussed, deposits of the second T-R cycle were almost completely removed by pre-Arenig erosion. Facies analysis of deposits of the first T-R cycle from the Kościerzyna and Gdańsk sections shows that the source areas of terrigenous material, during both transgressive and regressive phases of this cycle, were elevated zones of the East European Craton.
Źródło:
Geological Quarterly; 2000, 44, 3; 249-260
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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