Accepted author manuscript, 200 KB, PDF document
Available under license: CC BY-NC: Creative Commons Attribution-NonCommercial 4.0 International License
Final published version
Research output: Contribution to Journal/Magazine › Journal article › peer-review
<mark>Journal publication date</mark> | 1/10/2020 |
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<mark>Journal</mark> | Elements |
Issue number | 5 |
Volume | 16 |
Number of pages | 7 |
Pages (from-to) | 311-317 |
Publication Status | Published |
<mark>Original language</mark> | English |
A dvances in detrital noble gas thermochronometry by Ar-40/Ar-39 and (U-Th)/He dating are improving the resolution of sedimentary provenance reconstructions and are providing new insights into the evolution of Earth's surface. Detrital thermochronometry has the ability to quantify tectonic unroofing or erosion, temporal and dynamic connections between sediment source and sink, sediment lag-times and transfer rates, the timing of deposition, and postdepositional burial heating. Hence, this technique has the unique ability to use the detrital record in sedimentary basins to reconstruct Earth's dynamic long-term landscape evolution and how basins are coupled to their hinterlands.