Results 181 to 190 of about 3,499 (213)
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Geophysical Journal International, 2006
SUMMARY Results of palaeomagnetic investigations of the Lower Cretaceous teschenitic rocks in the Silesian unit of the Outer Western Carpathians in Poland bring evidence for pre-folding magnetization of these rocks. The mixed-polarity component reveals inclinations, between 56 ◦ and 69 ◦ , which might be either of Cretaceous or Tertiary age. Apparently
Jacek Grabowski
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SUMMARY Results of palaeomagnetic investigations of the Lower Cretaceous teschenitic rocks in the Silesian unit of the Outer Western Carpathians in Poland bring evidence for pre-folding magnetization of these rocks. The mixed-polarity component reveals inclinations, between 56 ◦ and 69 ◦ , which might be either of Cretaceous or Tertiary age. Apparently
Jacek Grabowski
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Cretaceous Research, 2011
Abstract Rich dinoflagellate cyst assemblages recorded from the Vendryne Formation, Tesin Limestone, and Hradiste Formation of the Silesian unit, Czech Republic are presented. The results of a qualitative and quantitative study of dinoflagellate cysts are presented and discussed.
Petr Skupien
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Abstract Rich dinoflagellate cyst assemblages recorded from the Vendryne Formation, Tesin Limestone, and Hradiste Formation of the Silesian unit, Czech Republic are presented. The results of a qualitative and quantitative study of dinoflagellate cysts are presented and discussed.
Petr Skupien
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Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 2006
The Moravo-Silesian zone is a zone with alpine-type tectonics with typical juxtaposition of nappe units defined by diferrent devonian facies.
Ondřej Bábek +4 more
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The Moravo-Silesian zone is a zone with alpine-type tectonics with typical juxtaposition of nappe units defined by diferrent devonian facies.
Ondřej Bábek +4 more
openaire +1 more source
Proceedings, 2012
The burial and thermal history of the Carboniferous gas source rocks in the Moravian-Silesian Unit (eastern part of the Fore-Sudetic Monocline, SW Poland) has been reconstructed by 1-D maturity modelling. It allowed to establish the timing of gas generation and expulsion in the Fore-Sudetic Monocline.
D. Botor +5 more
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The burial and thermal history of the Carboniferous gas source rocks in the Moravian-Silesian Unit (eastern part of the Fore-Sudetic Monocline, SW Poland) has been reconstructed by 1-D maturity modelling. It allowed to establish the timing of gas generation and expulsion in the Fore-Sudetic Monocline.
D. Botor +5 more
openaire +1 more source
Marine and Petroleum GeologyAAPG Bulletin, 2019
ABSTRACT The Węglówka oil field is located in the outer Carpathians. The outer Carpathians are a region where hydrocarbons were discovered and exploited at the end of the nineteenth century in several dozen oil fields, which are relatively small. The Węglówka oil field is one of the largest in this region.
Katarzyna Górniak
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ABSTRACT The Węglówka oil field is located in the outer Carpathians. The outer Carpathians are a region where hydrocarbons were discovered and exploited at the end of the nineteenth century in several dozen oil fields, which are relatively small. The Węglówka oil field is one of the largest in this region.
Katarzyna Górniak
exaly +2 more sources
Journal of Petroleum Geology
ABSTRACT This study represents the application of magnetic techniques in hydrocarbon prospection within the Outer Western Carpathian petroleum play, specifically focusing on the Eocene–Oligocene rocks of southeastern Poland. Magnetic minerals serve as a sensitive proxy for diagenetic processes, particularly concerning hydrocarbon ...
Maciej Łoziński +4 more
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ABSTRACT This study represents the application of magnetic techniques in hydrocarbon prospection within the Outer Western Carpathian petroleum play, specifically focusing on the Eocene–Oligocene rocks of southeastern Poland. Magnetic minerals serve as a sensitive proxy for diagenetic processes, particularly concerning hydrocarbon ...
Maciej Łoziński +4 more
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International Journal of Earth Sciences, 2013
The Main Ostrava Whetstone (MOW) is an important lithostratigraphic horizon of the Late Carboniferous sedimentary fill of the late Palaeozoic foreland Upper Silesian Basin. It is the largest and best-identified volcanogenic horizon in the basin, reaching thicknesses of 15.3 m and occupying an area of ca 2,973 km2 and a volume after lithification of 9 ...
Jirásek, Jakub +6 more
openaire +2 more sources
The Main Ostrava Whetstone (MOW) is an important lithostratigraphic horizon of the Late Carboniferous sedimentary fill of the late Palaeozoic foreland Upper Silesian Basin. It is the largest and best-identified volcanogenic horizon in the basin, reaching thicknesses of 15.3 m and occupying an area of ca 2,973 km2 and a volume after lithification of 9 ...
Jirásek, Jakub +6 more
openaire +2 more sources