Beo v1.0: numerical model of heat flow and low-temperature thermochronology in hydrothermal systems

Luijendijk, Elco

doi:https://doi.org/10.5194/gmd-12-4061-2019

Articles | Volume 12, issue 9

https://doi.org/10.5194/gmd-12-4061-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/gmd-12-4061-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 9

Model description paper

|

20 Sep 2019

Model description paper |

| 20 Sep 2019

Beo v1.0: numerical model of heat flow and low-temperature thermochronology in hydrothermal systems

Elco Luijendijk

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Final revised paper (published on 20 Sep 2019)
Preprint (discussion started on 04 Feb 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of “Beo v1.0: Numerical model of heat flow and low-temperature thermochronology in hydrothermal systems”, by Elco Luijendijk', Peter van der Beek, 19 Apr 2019
- AC2: 'Reply to review by Peter van der Beek', Elco Luijendijk, 02 Aug 2019
SC1: 'Review for gmd-2018-341', Manolis Veveakis, 15 May 2019
RC2: 'Review for Beo v1.0: Numerical model of heat flow and low-temperature thermochronology in hydrothermal systems Elco Luijendijk', Manolis Veveakis, 21 May 2019
- AC1: 'Reply to review by Manolis Veveakis', Elco Luijendijk, 31 Jul 2019

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Elco Luijendijk on behalf of the Authors (03 Aug 2019) Author's response Manuscript

ED: Publish as is (06 Aug 2019) by Thomas Poulet

Short summary

This paper presents a new model code that can be used to date the flow of hot fluids in the crust and the age of hot springs. It does so by modelling the thermal effects of fluid flow in the subsurface and by comparing the results with low-temperature thermochronology, which is a widely used method to quantify the temperature history of minerals and rocks. The model also demonstrates the effects of the depth and angle of permeable faults on temperatures of hot springs.