Articles | Volume 8, issue 2
https://doi.org/10.5194/gchron-8-373-2026
https://doi.org/10.5194/gchron-8-373-2026
Research article
 | 
12 Jun 2026
Research article |  | 12 Jun 2026

Extraction of multiple ages from c-axis projected fission tracks

Peter K. Jensen

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-6510', Raymond Donelick, 11 Feb 2026
    • AC1: 'Reply on RC1', Peter Klint Jensen, 04 Mar 2026
  • RC2: 'Comment on egusphere-2025-6510', Anonymous Referee #2, 14 Mar 2026
    • AC2: 'Reply on RC2', Peter Klint Jensen, 19 Mar 2026

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) (01 Apr 2026) by Shigeru Sueoka
AR by Peter Klint Jensen on behalf of the Authors (10 May 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 May 2026) by Shigeru Sueoka
RR by Anonymous Referee #2 (12 May 2026)
RR by Raymond Donelick (17 May 2026)
ED: Publish subject to technical corrections (18 May 2026) by Shigeru Sueoka
ED: Publish subject to technical corrections (18 May 2026) by Klaus Mezger (Editor)
AR by Peter Klint Jensen on behalf of the Authors (21 May 2026)  Author's response   Manuscript 
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Short summary
Natural fission of Uranium U-238 in minerals produce tracks in the crystal lattice. The density of tracks crossing the mineral surface is traditionally used together with the uranium concentration and the decay constant to calculate the age of fast-cooling minerals. A new equation is developed which includes the track length distribution of the tracks. It is then possible to age date the tracks as a function of their length. A detailed tectonic history of the minerals can then be derived.
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