Mélanges and broken formations at the boundary zone of the Magura and Silesian nappes (Gorlice area, Polish Outer Carpathians) : a result of sedimentary and tectonic processes

Starzec, K.; Malata, E.; Wronka, A.; Malina, L.

doi:10.7306/gq.1173

Artykuł - szczegóły

Tytuł artykułu

Mélanges and broken formations at the boundary zone of the Magura and Silesian nappes (Gorlice area, Polish Outer Carpathians) : a result of sedimentary and tectonic processes

Autorzy

Starzec K. , Malata E. , Wronka A. , Malina L.

Treść / Zawartość

Pełne teksty:

Starzec_K_Melages_Geol. Quart._Vol.59_No 1_2015.pdf

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Identyfikatory

DOI

10.7306/gq.1173

Warianty tytułu

Języki publikacji

Abstrakty

Based on geological ﬁeld mapping, analyses of cores from explanatory wells, and foraminiferal age control data, we have differentiated a few types of mélanges and broken formations at the bordering zone between the Magura and Silesian nappes (Gorlice area in the Polish Outer Carpathians). These mélanges and broken formations differ in composition and structure due to different settings and processes of their formation. Several levels of broken formation within the uppermost part of the Krosno Beds were formed as mass-transport deposits at the southern slope of the Silesian Basin. They may record tectonic pulses related to advancing accretionary wedge within Magura area and directly predate the stage of the larger-scale sedimentary mélange formation at the front of the wedge. This mélange is composed mainly of the material representing the Magura succession (Siary Subunit) and the Krosno type sediments of the Silesian succession. It was emplaced within the Silesian basin in the Early Miocene time. The so-called “Harklowa peninsula”, whose geological structure has been the subject of discussions and various interpretations in the past years, is built of this type of mélange. The other recognized type of broken formation and mélange represents the chaotic bodies formed at the base of the Magura Nappe.The results of our studies contribute to better understanding of the structural evolution of this part of the Outer Carpathians

Słowa kluczowe

tectonic and sedimentary mélange broken formation accretionary wedge Outer Carpathians foraminifera Early Miocene

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2015

Tom

Vol. 59, No. 1

Strony

169--178

Opis fizyczny

Bibliogr. 122 poz., rys., tab.

Twórcy

autor

Starzec K.

krzysztof.starzec@geokrak.pl

Geokrak sp. z o.o., Mazowiecka 21, 30-019 Kraków, Poland

autor

Malata E.

Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-063 Kraków, Poland

autor

Wronka A.

Geokrak sp. z o.o., Mazowiecka 21, 30-019 Kraków, Poland

autor

Malina L.

Geokrak sp. z o.o., Mazowiecka 21, 30-019 Kraków, Poland

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Uwagi

Fifth Polish Sedimentological Conference – POKOS V; Deep-sea flysch deposits – sedimentological aspects of the Carpathian basins history (2013; 16-19.05; Żywiec, Poland)

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Bibliografia

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