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. 2024 Feb 5;14:2964. doi: 10.1038/s41598-024-52935-2

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© The Author(s) 2024, corrected publication 2024

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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Characteristics of seismicity at Basel geothermal area. The epicentral distribution of the earthquakes is represented with a circle: grey dots represent earthquakes with $M_{W}$ less than 2, grey circles $M_{W}$ greater or equal to 2, and finally, the event with $M_{W}$ 3.1 is with red dots. The two upper insets show the location map of the Basel geothermal area and the seismic monitoring network. The lower inset shows the magnitude temporal distribution, the symbols are coloured according to the depth. The figures are generated by using the version 5 of Generic Mapping Tools (https://www.generic-mapping-tools.org/).