Mariusz Paszkowski
Polish Academy of Sciences
SedimentologyDevonianGeomorphologyMicroprobeSedimentary depositional environmentGeologyDiagenesisPaleozoicClastic rockContinental crustFaciesCratonCarboniferousPaleontologyOil shaleMassifGeochemistryMaterials scienceMineralogySedimentary basinGeochronologyMonaziteBalticaSuture (geology)ZirconEast European CratonGoniatitesProvenanceCarbonateIsochronPeatSedimentary rockProterozoicSiliciclastic
38Publications
10H-index
319Citations
Publications 36
Newest
#1K. Dudzisz (PAN: Polish Academy of Sciences)
#2Marek Lewandowski (PAN: Polish Academy of Sciences)H-Index: 17
Last. Maciej J. Bojanowski (PAN: Polish Academy of Sciences)H-Index: 10
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Abstract This study addresses new paleomagnetic, geochemical, mineralogical, and rock-magnetic data from four drill cores of the western part of the East European Craton, representing mainly siliciclastics supplemented by volcaniclastics and a few basaltic rock samples. The cores comprise Mesoproterozoic samples of 1400–1030 Ma and Neoproterozoic (Ediacaran) samples of 588–541 Ma. According to the magnetic data, the dominant magnetic carrier in basalts is magnetite, while two genetic types of he...
3 CitationsSource
#2Andrew J. BigginH-Index: 25
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The Devonian, like much of the Paleozoic, has long been a problematic period for paleomagnetism. Devonian paleomagnetic data are generally difficult to interpret and have complex partial or full overprints; problems that arise in data obtained from both sedimentary and igneous rocks. As a result, the reconstruction of tectonic plate motions, performed largely using apparent polar wander paths, has large uncertainty. Similarly, the Devonian geomagnetic polarity time scale is very poorly constrain...
Source
#2Andrew J. BigginH-Index: 25
Last. Richard K. BonoH-Index: 9
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Source
#1Agnieszka Pisarzowska (University of Silesia in Katowice)H-Index: 10
#2Michał Rakociński (University of Silesia in Katowice)H-Index: 14
Last. Manfred GerekeH-Index: 1
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Abstract A wide range of various proxies (e.g., mineralogy, organic carbon, inorganic geochemistry, C and Mo isotopes, and framboidal pyrite) were applied for interpretation of changing oceanic redox conditions, bioproductivity, and the regional history of volcanic activity. This resulted in internally consistent interpretation of the late Famennian Hangenberg Crisis in subtropical deepest water sites of the epeiric Rhenohercynian and Saxo–Thuringian basins, as well as more open sites of the Pal...
9 CitationsSource
#1Mariusz Paszkowski (PAN: Polish Academy of Sciences)H-Index: 10
#2Bartosz Budzyń (PAN: Polish Academy of Sciences)H-Index: 11
Last. Agnieszka Pisarzowska (PAN: Polish Academy of Sciences)H-Index: 10
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Abstract The sedimentary cover of the East European Craton (EEC) is unique because of its low degree of diagenetic alteration that allows preservation of the original “source to sink” relationships. The present study provides U-Pb and Hf zircon data for the entire Proterozoic sedimentary section of the EEC based on samples from five boreholes in Belarus within the Volyn-Orsha Basin, one of the most important sedimentary basins of the craton. Twenty-one samples of mudstones and sandstones were se...
13 CitationsSource
#1Katarzyna Kołtonik (PAN: Polish Academy of Sciences)H-Index: 3
#2Peter E. Isaacson (UIdaho: University of Idaho)H-Index: 16
Last. Wojciech Krawczyński (University of Silesia in Katowice)H-Index: 8
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Abstract The Toregua Formation in northern Bolivia comprises a continuous succession of sedimentary rocks containing two glacial intervals related to the onset of the Late Paleozoic Ice Age (LPIA). The provenance and depositional tectonic setting of the Upper Devonian–Mississippian (lower) and Pennsylvanian (upper) glacial intervals are separated by non-glacial deposits observed in the Manuripi X-1 and Pando X-1 drill cores, from which petrography, geochemistry, detrital zircon U Pb and monazite...
6 CitationsSource
#1Katarzyna Kołtonik (PAN: Polish Academy of Sciences)H-Index: 3
#2Agnieszka Pisarzowska (PAN: Polish Academy of Sciences)H-Index: 10
Last. Wolfgang Franke (Goethe University Frankfurt)H-Index: 9
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1 CitationsSource
#1Szczepan J. Porębski (AGH University of Science and Technology)H-Index: 11
#2Robert Anczkiewicz (PAN: Polish Academy of Sciences)H-Index: 22
Last. Z. Mikołajewski (Southern California Gas Company)H-Index: 1
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11 CitationsSource
#1Karol Jewuła (PAN: Polish Academy of Sciences)H-Index: 5
#2Michał Matysik (Jagiellonian University)H-Index: 5
Last. Joachim Szulc (Jagiellonian University)H-Index: 16
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Abstract The numerous discoveries of disintegrated skeletons of large terrestrial vertebrates within several thin levels of the Upper Silesian Keuper initiated broad investigations into the palaeoenvironment and age of the bone-bearing sediments. Despite years of research, the depositional history of the Upper Triassic continental succession and its controlling factors are still poorly recognized. This paper reconstructs the depositional evolution of the Upper Triassic strata in Upper Silesia, P...
10 CitationsSource