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

Widera, Marek; Stawikowski, Wojciech; Uścinowicz, Grzegorz

doi:10.24425/agp.2019.126439

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Tytuł artykułu

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

Autorzy

Widera Marek , Stawikowski Wojciech , Uścinowicz Grzegorz

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DOI

10.24425/agp.2019.126439

Warianty tytułu

Języki publikacji

Abstrakty

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.

Słowa kluczowe

Palaeozoic Platform Polish Basin salt diapirism synsedimentary tectonics lignite compaction

platforma paleozoiczna basen polski diapiryzm solny wysad solny tektonika synsedymentacyjna zagęszczanie węgla brunatnego

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2019

Tom

Vol. 69, no. 3

Strony

387--401

Opis fizyczny

Bibliogr. 61 poz., rys.

Twórcy

autor

Widera Marek

widera@amu.edu.pl

Institute of Geology, Adam Mickiewicz University, 12 Krygowski Street, 61-680 Poznań, Poland

autor

Stawikowski Wojciech

wojst@amu.edu.pl

Institute of Geology, Adam Mickiewicz University, 12 Krygowski Street, 61-680 Poznań, Poland

autor

Uścinowicz Grzegorz

gusc@pgi.gov.pl

Polish Geological Institute-National Research Institute, Marine Geology Branch, 5 Kościerska Street, 80-328 Gdańsk, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

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Bibliografia

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