Surface exposure dating with cosmogenic nuclides

In the last decades surface exposure dating using cosmogenic nuclides has emerged as a powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic nuclides are produced in rocks and sediment due to reactions induced by cosmic rays. Landforms ranging in age from a few hundre...

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Main Authors: S. Ivy-Ochs, F. Kober
Format: Article
Language:deu
Published: Copernicus Publications 2008-08-01
Series:Eiszeitalter und Gegenwart
Online Access:https://www.eg-quaternary-sci-j.net/57/179/2008/egqsj-57-179-2008.pdf
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author S. Ivy-Ochs
F. Kober
author_facet S. Ivy-Ochs
F. Kober
author_sort S. Ivy-Ochs
collection DOAJ
description In the last decades surface exposure dating using cosmogenic nuclides has emerged as a powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic nuclides are produced in rocks and sediment due to reactions induced by cosmic rays. Landforms ranging in age from a few hundred years to tens of millions of years can be dated (depending on rock or landform weathering rates) by measuring nuclide concentrations. In this paper the history and theory of surface exposure dating are reviewed followed by an extensive outline of the fields of application of the method. Sampling strategies as well as information on individual nuclides are discussed in detail. The power of cosmogenic nuclide methods lies in the number of nuclides available (the radionuclides 10Be, 14C, 26Al, and 36Cl and the stable noble gases 3He and 21Ne), which allows almost every mineral and hence almost every lithology to be analyzed. As a result focus can shift to the geomorphic questions. It is important that obtained exposure ages are carefully scrutinized in the framework of detailed field studies, including local terrace or moraine stratigraphy and regional morphostratigraphic relationships; as well as in light of independent age constraints.
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spelling doaj.art-01f99b91ea064deeb40e2b2333c00e0a2022-12-21T18:14:52ZdeuCopernicus PublicationsEiszeitalter und Gegenwart0424-71162199-90902008-08-015717920910.3285/eg.57.1-2.7Surface exposure dating with cosmogenic nuclidesS. Ivy-OchsF. KoberIn the last decades surface exposure dating using cosmogenic nuclides has emerged as a powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic nuclides are produced in rocks and sediment due to reactions induced by cosmic rays. Landforms ranging in age from a few hundred years to tens of millions of years can be dated (depending on rock or landform weathering rates) by measuring nuclide concentrations. In this paper the history and theory of surface exposure dating are reviewed followed by an extensive outline of the fields of application of the method. Sampling strategies as well as information on individual nuclides are discussed in detail. The power of cosmogenic nuclide methods lies in the number of nuclides available (the radionuclides 10Be, 14C, 26Al, and 36Cl and the stable noble gases 3He and 21Ne), which allows almost every mineral and hence almost every lithology to be analyzed. As a result focus can shift to the geomorphic questions. It is important that obtained exposure ages are carefully scrutinized in the framework of detailed field studies, including local terrace or moraine stratigraphy and regional morphostratigraphic relationships; as well as in light of independent age constraints.https://www.eg-quaternary-sci-j.net/57/179/2008/egqsj-57-179-2008.pdf
spellingShingle S. Ivy-Ochs
F. Kober
Surface exposure dating with cosmogenic nuclides
Eiszeitalter und Gegenwart
title Surface exposure dating with cosmogenic nuclides
title_full Surface exposure dating with cosmogenic nuclides
title_fullStr Surface exposure dating with cosmogenic nuclides
title_full_unstemmed Surface exposure dating with cosmogenic nuclides
title_short Surface exposure dating with cosmogenic nuclides
title_sort surface exposure dating with cosmogenic nuclides
url https://www.eg-quaternary-sci-j.net/57/179/2008/egqsj-57-179-2008.pdf
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