Articles | Volume 1, issue 1
https://doi.org/10.5194/gchron-1-17-2019
https://doi.org/10.5194/gchron-1-17-2019
Research article
 | 
26 Sep 2019
Research article |  | 26 Sep 2019

Resolving the effects of 2-D versus 3-D grain measurements on apatite (U–Th) ∕ He age data and reproducibility

Emily H. G. Cooperdock, Richard A. Ketcham, and Daniel F. Stockli

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to technical corrections (26 Aug 2019) by Cecile Gautheron
ED: Publish subject to technical corrections (26 Aug 2019) by Greg Balco (Editor)
AR by Emily Cooperdock on behalf of the Authors (02 Sep 2019)  Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Emily Cooperdock on behalf of the Authors (23 Sep 2019)   Author's adjustment   Manuscript
EA: Adjustments approved (23 Sep 2019) by Cecile Gautheron
Download
Short summary
(U–Th) / He chronometry relies on accurate grain-specific size and shape measurements. Using > 100 apatite grains to compare assumed 2-D versus true 3-D grain shapes measured by a microscope and X-ray computed tomography, respectively, we find that volume and surface area both differ by ~ 25 % between the two techniques and directly affect mass and concentration measurements. But we found a very small effect on the FT correction (2 %) and no discernible impact on mean sample age or dispersion.