Sudety w kenozoiku : od tektonicznej ekshumacji podłoża do współczesnej rzeźby – wnioski z termochronologii niskotemperaturowej

Sobczyk, Artur

doi:10.7306/2025.86

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Sudety w kenozoiku : od tektonicznej ekshumacji podłoża do współczesnej rzeźby – wnioski z termochronologii niskotemperaturowej

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Sobczyk Artur

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Sobczyk_A_Sudety_P. Geol._Vol. 73_nr 9_2025.pdf

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DOI

10.7306/2025.86

Warianty tytułu

The Sudetes in the Cenozoic era : from tectonic bedrock exhumation to the modern landscape – insights from low-temperature thermochronology

Języki publikacji

Abstrakty

Low-temperature the rmochronology based on apatite and zircon (40-240°C) provides essential infor¬mation on the evolution of the Sudetes during the Mesozoic and Cenozoic. AFT data from various areas of the Sudetes indicate intense cooling and basement exhumation during the Late Cretaceous-Paleogene (~90-45 Ma). The estimated mean exhumation rate during this period varied between 1.0 and 0.04 km/Ma. In the Cenozoic, there was a significant slowdown in tectonic processes and a decrease in the exhumation rate to <0.01 km/Ma. Results from numerical modelling of AFT data suggest that the folding of Cretaceous sediments in the lntra-Sudetic Synclinorium and the Upper Nysa Kłodzka Graben took place between 75 and 70 Ma. Thermochronology has also provided evidence of deep burial of the Sudetes in the Late Cretaceous, with the observed thermal reset suggesting that the thickness of the sedimentary cover may have reached up to 6 km. The development of the Sudetic landscape into a form similar to the present one did not occur earlier than after the Eocene, when the last phase of basement rock cooling and associated denudation of the Me¬ta-Carpathian Swell was recorded. The final uplift of the Sudetic Block began in the Middle Miocene (15±5 Ma), and the total erosion over the past 90 million years reached 5-6 km.

Słowa kluczowe

metoda helowa i trakowa (U-Th)/ He modelowanie historii termicznej tektonika Masyw Czeski Północno-Wschodni Południowo-Zachodnia Polska

fission-track analysis (U-Th)/He dating thermal history modelling tectonics NE Bohemian Massif SW Poland

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Przegląd Geologiczny

Rocznik

2025

Tom

Vol. 73, nr 9

Strony

804--812

Opis fizyczny

Bibliogr. 65 poz., tab., wykr.

Twórcy

autor

Sobczyk Artur

artur.sobczyk@uwr.edu.pl

Instytut Nauk Geologicznych, Uniwersytet Wrocławski, pl. M. Borna 9, 50-204 Wrocław

https://orcid.org/0000-0003-3829-561X

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