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Thermochronology on Sand and Sandstones for Stratigraphic and Provenance Studies

  • Andrew Carter
Chapter
Part of the Springer Textbooks in Earth Sciences, Geography and Environment book series (STEGE)

Abstract

Clastic detritus preserved within a sedimentary basin represents a natural reservoir of geological information that can be used to constrain sediment deposition age and develop a picture of the sediment routing system and source terrain(s) in terms of location, age, composition and tectonic and climate stability. This chapter charts the development and applications of fission-track (FT) analysis to solve stratigraphic and provenance problems. Many of the interpretative tools and strategies developed for FT data are also applicable to detrital (U–Th)/He and other geochronological data. Provenance interpretations based on double and triple-dating strategies may be further improved by combining with mineral trace element data.

Notes

Acknowledgements

The author thanks Dave Chew, Alberto Resentini (Fig. 14.4) and Marco G. Malusà for their timely and constructive reviews.

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Authors and Affiliations

  1. 1.Department of Earth and Planetary Sciences, BirkbeckUniversity of LondonLondonUK

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