Preprints
https://doi.org/10.5194/egusphere-2025-5806
https://doi.org/10.5194/egusphere-2025-5806
10 Dec 2025
 | 10 Dec 2025
Status: this preprint is open for discussion and under review for Solid Earth (SE).

Interpreting the cause of bound earthquakes at underground injection experiments

Ryan Schultz, Linus Villiger, Valentin Gischig, and Stefan Wiemer

Abstract. Constraining the maximum possible magnitude (MMAX) of an induced earthquake sequence is a challenging process with important implications for managing risks. CAP-tests are a suite of statistical tests that can infer, quantify, and select best-fitting MMAX models via an earthquake catalogue’s magnitudes. We use CAP-tests to discern between bound/unbound earthquake sequences at underground laboratories, where high-resolution and near-field geophysical observations are abundant. There, we find clear evidence for bound sequences, where magnitude growth was restricted during stimulation. Furthermore, bound sequences tend to be associated with stimulations that occurred within intact rock. On the other hand, unbound sequences tended to be associated with stimulations where hydraulic fractures interacted with relatively large pre-existing faults/fractures. We further examine bound sequences by fitting magnitude growth to a generalized family of MMAX functions. This process appears to be able to aggregate bound sequences into categories consistent with theoretical considerations (e.g., tectonic, tensile-crack, or shear-crack). These results provide a basis for validating and interpreting bound sequences in controlled experiments, which is important for extrapolating to larger-scale observations. Overall, CAP-tests appear to be a promising avenue for constraining MMAX from earthquake catalogue data.

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Ryan Schultz, Linus Villiger, Valentin Gischig, and Stefan Wiemer

Status: open (until 21 Jan 2026)

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Ryan Schultz, Linus Villiger, Valentin Gischig, and Stefan Wiemer
Ryan Schultz, Linus Villiger, Valentin Gischig, and Stefan Wiemer
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Short summary
We use statistical tests to infer MMAX from an earthquake catalogue and focus on data from three underground laboratories with controlled injection experiments. There, we find clear evidence for MMAX bounds and corroborate interpretations of fracture growth against other geophysical studies.  Unbound sequences occur when stimulation is directed towards pre-existing faults. The validation of our methods against well-studied cases is encouraging and will help validate future interpretations.
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