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. 2022 Feb 8;12:2065. doi: 10.1038/s41598-022-06067-0

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© The Author(s) 2022

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Temperature and pressure evolutions. Spatial distribution of temperature (a) and pore pressure (b) after 30 years of fluid circulation in a geothermal doublet in a HSA surrounded by low-permeable faults. The evolution with time of temperature (c) and pressure (d) at the reinjection and production wells.