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Triassic-Jurassic evolution of the Pomeranian segment of the Mid-Polish Trough-basement tectonics and subsidence patterns

Autorzy
Krzywiec P.
Treść / Zawartość
Pełne teksty:
krzywiec_triassic_1_2006.pdf
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Based on reflection seismic data, a regional tectonicmodel was constructed for the sub-Zechstein basement of the Pomeranian (NW) segment of theMid-Polish Trough (MPT). This model is based on the concept that the thick Zechstein salts acted on a basin-wide scale as a mechanical decoupling layer during the Mesozoic evolution of the MPT. Due to this regional decoupling effect, Mesozoic extensional faulting was mostly restricted to the sub-Zechstein salt basement whilst normal faulting played a subordinate role in the Mesozoic syn-extensional sedimentary series characterized by gradual lateral thickness changes. Locally, normal faulting affecting Mesozoic series triggered the development of salt diapirs. Mechanical decoupling ofMesozoic series fromtheir pre-Zechstein substratum played also an important role during the Late Cretaceous-Paleogene inversion of the Mid-Polish Trough. Taking into account: 1— the location of Mesozoic thickness gradients, 2—the structural configuration of the sub-Zechstein basement, and 3—the location of salt structures, a tectonic map was constructed showing the inferred sub-salt fault zones that were active during the subsidence and inversion of the Pomeranian part of the MPT. A high degree of correlation was achieved between the seismically mapped regional sub-salt structural patterns and magnetic and gravity features, as well as the main inversion structures. Moreover, a very good correlation was established between the inferred basement fault zones and the gross thickness patterns of the Triassic-Jurassic successions. The NE boundary of theMPT was generally controlled by the SW margin of the East European Craton, whilst its SW boundary coincides with a system of fault zones most probably inherited from earlier tectonic phases. Contrary to previous hypotheses, there is no evidence for important strike-slip faulting transverse to the main axis of the Pomeranian segment of the MPT.
Słowa kluczowe
EN
Wydawca
Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
Czasopismo
Geological Quarterly
Rocznik
2006
Tom
Vol. 50, No. 1
Strony
139--150
Opis fizyczny
mapki, wykr., bibliogr. 92 poz.
Twórcy
autor
Krzywiec P.
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Bibliografia
Identyfikator YADDA
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