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. 2022 Aug 17;12:14000. doi: 10.1038/s41598-022-18130-x

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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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MFFI comparison to ATHP accelerometer. (Left) A map of Greece showing in a red box the location of MFFI system and ATHP accelerometric station (the inset magnifies the area contained in the rectangular frame) and the epicenters with black stars of earthquakes selected for analysis in the present study. (Right) Comparison of the time series collected by MFFI and ATHP regarding the earthquake taking place east of Crete Island (October 12, 2021, 09:24:03 UTC, Crete (ML = 6.3)). Pg/Sg, Pn/Sn theoretical arrival times are marked with blue dotted lines for reference. Map on the left has been created using open software GMT ver 5.4 (https://www.generic-mapping-tools.org/).