Articles | Volume 3, issue 2
https://doi.org/10.5194/gchron-3-561-2021
https://doi.org/10.5194/gchron-3-561-2021
Research article
 | 
21 Dec 2021
Research article |  | 21 Dec 2021

Deconvolution of fission-track length distributions and its application to dating and separating pre- and post-depositional components

Peter Klint Jensen and Kirsten Hansen

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (16 Jun 2021) by Shigeru Sueoka
AR by Peter Klint Jensen on behalf of the Authors (26 Jul 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Jul 2021) by Shigeru Sueoka
RR by Anonymous Referee #3 (14 Sep 2021)
ED: Publish subject to revisions (further review by editor and referees) (14 Sep 2021) by Shigeru Sueoka
AR by Peter Klint Jensen on behalf of the Authors (25 Oct 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Oct 2021) by Shigeru Sueoka
RR by Anonymous Referee #3 (05 Nov 2021)
ED: Publish subject to technical corrections (08 Nov 2021) by Shigeru Sueoka
ED: Publish subject to technical corrections (10 Nov 2021) by Greg Balco (Editor)
AR by Peter Klint Jensen on behalf of the Authors (14 Nov 2021)  Author's response   Manuscript 
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Short summary
Fission tracks are generated in minerals due to spontaneous fission of uranium-238. The initial track length decreases with time due to recrystallization. The age of a track can be calculated by counting the number of the shorter tracks per volume and including the decay constant. However, the theoretical order of the track length versus time is disrupted by uncertainties. We shown how the order can be re-established. The age of tectonic events such as uplift and burial can then be determined.