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2019 | OriginalPaper | Chapter

15. Exhumation Studies of Mountain Belts Based on Detrital Fission-Track Analysis on Sand and Sandstones

Author : Matthias Bernet

Published in: Fission-Track Thermochronology and its Application to Geology

Publisher: Springer International Publishing

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Abstract

Fission-track (FT) analysis of detrital apatite and zircon from modern sediments and ancient sandstone is a commonly used approach for studying and quantifying the long-term exhumation history of convergent mountain belts. Being aware of potential bias in the age spectra because of sampling, sample preparation and statistical data treatment such as peak-fitting, FT ages from sediments and sedimentary rocks of known depositional age can be readily transferred into long-term average exhumation or erosion rates using the lag-time concept. Double dating of single grains with the FT and U–Pb methods provides additional valuable provenance information, for example, for identifying volcanically derived grains, which may obscure the exhumation signal. Applying both apatite and zircon FT dating on the same samples allows combining the study of source area exhumation and the thermal evolution of sedimentary basins.

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previous chapter Thermochronology on Sand and Sandstones for Stratigraphic and Provenance Studies

next chapter A Guide for Interpreting Complex Detrital Age Patterns in Stratigraphic Sequences

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Title: Exhumation Studies of Mountain Belts Based on Detrital Fission-Track Analysis on Sand and Sandstones
Author: Matthias Bernet
Publisher: Springer International Publishing
Book: Fission-Track Thermochronology and its Application to Geology
Print ISBN: 978-3-319-89419-5

Electronic ISBN: 978-3-319-89421-8

Copyright Year: 2019
DOI: https://doi.org/10.1007/978-3-319-89421-8_15