Erosional history of the Karkonosze Granite Massif : constraints from adjacent sedimentary basins and thermochronology

Migoń, P.; Danišík, M.

doi:10.7306/gq.1032

Artykuł - szczegóły

Tytuł artykułu

Erosional history of the Karkonosze Granite Massif : constraints from adjacent sedimentary basins and thermochronology

Autorzy

Migoń P. , Danišík M.

Treść / Zawartość

Pełne teksty:

Migon_P_Erosional_GQ_Vol.56_No.3_2012.pdf

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Identyfikatory

DOI

10.7306/gq.1032

Warianty tytułu

Języki publikacji

Abstrakty

The long-term erosional history of the Karkonosze Granite Massif is revised and reconstructed using different sources of information, including the sedimentary record of adjacent basins, previously published low-temperature thermochronological data and geomorphic features. Although the evidence is still incomplete, this work has identified a number of intervals, of unequal duration, characterized by different denudation regimes and rates. Several major phases of rapid exhumation are inferred - in the Permian and the Early Triassic as seen in the sedimentary record, and in the Late Cretaceous as shown by both the thermochronological and sedimentary records. Neotectonic uplift of the Karkonosze Mts. in the late Cenozoic is not recorded in the thermochronological record and there is no evidence of any accelerated denudation close to the massif. Apatite fission track data show that >~3.6 km of rock must have been eroded since the Turonian, while the results of zircon (U-Th)/He analysis suggest that in places erosion of >~6 km of rock must have taken place. This picture differs from previous estimates of denudat ion which suggested that only 2-2.5 km has been eroded from the axial part of the Karkonosze dome since the exposure of granite batholith in the Permian.

Słowa kluczowe

Karkonosze Sudetes erosional history thermochronology sedimentary basins

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2012

Tom

Vol. 56, No 3

Strony

441--456

Opis fizyczny

Biblogr. 102 poz., rys., wykr.

Twórcy

autor

Migoń P.

piotr.migon@uni.wroc.pl

Department of Geography and Regional Development, University of Wrocław, Uniwersytecki 1, 50-137 Wrocław, Poland

autor

Danišík M.

m.danisik@waikato.ac.nz

John de Laeter Centre of Mass Spectrometry, Applied Geology, Curtin University of Technology, GPO Box U1987, Perth WA 6845, Australia
Department of Earth and Ocean Sciences, The University of Waikato, Private Bag 3105, Hamilton 3240, New Zealand

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