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Wyszukujesz frazę "Radkovets, N." wg kryterium: Autor


Wyświetlanie 1-3 z 3
Tytuł:
The Silurian of southwestern margin of the East European Platform (Ukraine, Moldova and Romania) : lithofacies and palaeoenvironments
Autorzy:
Radkovets, N.
Powiązania:
https://bibliotekanauki.pl/articles/2059822.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
East European Platform
Silurian
lithofacies
reef
shelf of Baltica
palaeoenvironments
Opis:
Silurian strata, stretching along the western margin of the East European Platform from the Baltic to the Black Sea, represent a potential target for both conventional and unconventional hydrocarbon exploration. Distribution of the black shale facies, prospective for shale gas, and the reef facies, prospective for oil, has been studied in respect of palaeoenvironments. The Silurian sequence has been investigated in the territory of Ukraine (Volyn-Podillyan Plate, Dobrogean Foredeep) and correlated with the data on Moldova and Romania (Moldovian Platform). The occurrence of Silurian strata, their thickness, and petrographic and lithological characteristics allowed reconstructing the distribution of open-shelf, reef and lagoonal facies. The reef facies migrated during the Wenlock–Middle Pridoli, shifting towards the open sea and back towards the shore, and therefore has been termed a migrating reef facies. Correspondingly, the boundary between the open-shelf and reef facies was shifting. The facies distribution was controlled by the transgressive-regressive cycles, which caused the fluctuations of the shelf water depth in different time intervals of the Silurian. The shelf water depth of about 100 m, where the top of the oxygen-minimum layer impinged on the sea bottom, was the boundary between the open-shelf facies, represented by organic-rich sediments, and the reef buildups.
Źródło:
Geological Quarterly; 2015, 59, 1; 105--118
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Cechy litologiczne i geochemiczne turońskich osadów węglanowych ze stylolitami Karpat pokucko-bukowińskich
Lithological and geochemical features of Turonian carbonates with stylolites in Pokuttya–Bukovyna (Ukrainian Carpathians)
Autorzy:
Radkovets, N.
Manzhar, N.
Powiązania:
https://bibliotekanauki.pl/articles/2062203.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Turonian limestones
stylolites
material compositions
Carpathian autochthon
wapienie turonu
stylolity
skład mineralny
autochton karpacki
Opis:
Badania składu materialnego węglanów ze stylolitami w Karpatach pokucko-bukowińskich wykazały, że zawartość CaCO3 w skałach waha się od 68 do 92%, a pozostałości nierozpuszczalnej od 8 do 32. Szczątki organiczne wielkości od 0,02 do 1 mm (otwornice, ślimaki, ramienionogi i inoceramy) stanowią 40–55% skały, a reszta to kalcyt pelitomorficzny. Części nierozpuszczalne materiału stylolitów to na ogół minerał hydromikowy – illit oraz materia organiczna, cechująca się zwiększoną zawartością żelaza i strontu (>10 razy). Spektoskopia infraczerwona bituminu chloroformowego zawartego w stylolitach wykazała, że materia organiczna powstała głównie z mikroskładników planktonicznych (autochtonicznych) i uległa istotnym zmianom postsedymentacyjnym: polimeryzacji oraz utleniania.
Chemical analysis of carbonates with stylolites from the autochthon of the Pokuttya–Bukovyna Carpathians showed that the СаСО3 content in the rocks ranges between 68 and 92%, insoluble residue makes 8–32%. Investigation of clayey limestones using the polarizing microscopy allowed to establish that the 0.02–1 mm sized organic debris (foraminifera, gastropods, brachiopods and inocerams) makes 40–55% of the rock. The rest is the matrix represented by pelitomorphic calcite. X-ray diffractometry showed that insoluble residue of the organic-rich clay from stylolites is represented by the hydromicaceous mineral – illite with admixture of organic matter. Results of quantitative spectral analysis revealed the increased iron and strontium (>10 times) content in both limestones and organic-rich clays. Infrared spectrometry of chloroform bitumen extracted from the organic-rich clay from stylolites showed that the dispersed organic matter by its origin consists mainly of planktonogenic (autochthonous) microcomponents and underwent significant postsedimentary transformations: polymerization and oxidation.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2012, 449; 131--136
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ediacaran-Paleozoic subsidence history of the Volyn-Podillya-Moldavia Basin (W and SW Ukraine, Moldova, NE Romania)
Autorzy:
Poprawa, P.
Radkovets, N.
Rauball, J.
Powiązania:
https://bibliotekanauki.pl/articles/2060431.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Ediacaran-Early Paleozoic
Volyn-Podillya-Moldavia basin
tectonic subsidence
backstripping
Opis:
Tectonic subsidence history was analysed for the Ediacaran-Paleozoic Volyn-Podillya-Moldavia Basin, by performing 1D backstripping for 21 boreholes located in western and SW Ukraine, Moldova and NE Romania. Tectonic subsidence history is coherent across the area studied. Development of the basin commenced with an Ediacaran phase of extension, initiated with the emplacement of rift-related volcanic rocks and associated with rapid syn-rift tectonic subsidence. During this event, tectonic subsidence increased towards the SW, i.e. towards the edge of the East European Craton, where the Ediacaran rift zone was located. At that time, a rift developed along the whole SW margin of the East European Craton from Scandinavia to the Black Sea. Development of this large extensional basin was related to the latest stages of break-up of the Precambrian supercontinent Rodinia/Pannotia and ultimately the formation of the Tornquist Ocean. The latest Ediacaran to Late Ordovician tectonic subsidence pattern was characteristic of the post-rift thermal sag stage of extensional basins. The SW margin of the newly formed Baltica, including the area studied, became a passive continental margin. The late Cambrian uplift and erosion was presumably related to a far-field effect of contractional events or intra-plate stresses. Since the Late Ordovician, a gradual change to a collisional tectonic setting is observed across the SW margin of Baltica. In the study area, this is indicated by a systematic increase in subsidence rate from Wenlock to Early Devonian time, creating subsidence curves with convex shapes typical of foreland basin development. The Silurian to Early Devonian Volyn-Podillya-Moldavia Basin is interpreted here as a flexural foredeep related to a Caledonian collision zone located further to the SW. The prominent diachroneity in the initiation of the foredeep basin development at a scale of the whole SW margin of Baltica is coherent with a model of oblique collision of Avalonia and Baltica. During the Pragian-Emsian, the basin was part of a system of post-collisional Old Red basins, with subsidence driven presumably by lithospheric isostatic imbalance resulting from the Caledonian collision and development of an accretionary wedge. Middle to Late Devonian short-term phases of rapid subsidence in small depocentres might be regarded as an indication of a transtensional tectonic regime.
Źródło:
Geological Quarterly; 2018, 62, 3; 459--486
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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