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Paleogene-Neogene tectonic evolution of the lignite-rich Szamotuły Graben

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Szamotuły Graben covers the southernmost part of the Permo-Mesozoic Poznań–Szamotuły Fault Zone. Along this regional discontinuity there are several salt structures, including the Szamotuły diapir, over which an extensional graben formed in the Paleogene and Neogene. The graben is located north of Poznań in central-western Poland, and is NW–SE-trending, ~20 km long, 3–5.5 km wide, and up to 160 m deep. It is filled with Lower Oligocene and Neogene sediments, including relatively thick lignite seams. Data from boreholes allow the assignment of the graben-fill sediments to appropriate lithostratigraphic units. Furthermore, analysis of changes in the thickness of these units provides evidence for periods of accelerated graben subsidence or uplift relative to its flanks. As a result, two distinct stages of tectonic subsidence and one inversion in the Paleogene–Neogene evolution of the Szamotuły Graben have been distinguished. Thus, relatively significant subsidence occurred in the Early Oligocene and the middle Early–earliest Mid-Miocene, while slight inversion took place in the middle part of the Mid-Miocene.
Rocznik
Strony
387--401
Opis fizyczny
Bibliogr. 61 poz., rys.
Twórcy
autor
  • Institute of Geology, Adam Mickiewicz University, 12 Krygowski Street, 61-680 Poznań, Poland
  • Institute of Geology, Adam Mickiewicz University, 12 Krygowski Street, 61-680 Poznań, Poland
  • Polish Geological Institute-National Research Institute, Marine Geology Branch, 5 Kościerska Street, 80-328 Gdańsk, Poland
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Uwagi
PL
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-aa8a9b61-6fae-40f1-99ea-eea170a28a3a
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