Analysis uncovers fault parameters using InSAR time series, indicating a low static friction coefficient in Argentina's mid-crustal structures.
Summary On January 18, 2021, a blind mid-crustal Mw ∼6.4 earthquake occurred near San Juan, Argentina. The observation of associated ground deformation with single interferograms is obscured by strong tropospheric signals. We apply appropriate corrections to the data and reconstruct the deformation field associated to the event through InSAR time series approach. We show it is possible to retrieve this signal to invert the fault parameters. The observed ground deformation is consistent with a high angle NW-dipping fault plane at a centroid depth of ∼19 km. The geometry of this fault supports the reactivation of pre-existing structures within the Cuyania Terrane, suggesting a direct structural connection and strain transfer to the actively deforming, east-vergent Precordillera front. We analyze our findings to deduce a static friction coefficient ≤0.3 for mid-crustal faults of the region.
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León-Ibáñez et al. (2025) studied this question.
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