Timoshenko Flexocompression Beam Analogy Applied to the Calculation of Seismogenic Thickness and Cortical Rupture Prediction in the Sierra de Pie de Palo

This paper presents a deterministic geomechanical model to parameterize the spatial variabilityof seismogenic thickness (h) in basement thrust faults under flat-slab subduction regimes. We developa physico-mathematical analogy by transforming the elemental elastic approximation into avariable cross-section Timoshenko beam model subjected to tectonic flexocompression. The governingdifferential equations are solved numerically over a regularized mesh using interseismic strainrates derived from GPS data. The lower seismogenic boundary (zmax) is formulated by coupling theeffective stress tensor, deep dehydration-induced pore pressure, and rheological constitutive equations.The model is quantitatively calibrated and validated against hypocentral depths recorded byINPRES, and its integration into probabilistic seismic hazard assessment schemes is discussed

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-06-27
DOI
https://doi.org/10.5281/zenodo.20947413
Primary Topic
earthquake and tectonic studies
Type
preprint
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preprint

Timoshenko Flexocompression Beam Analogy Applied to the Calculation of Seismogenic Thickness and Cortical Rupture Prediction in the Sierra de Pie de Palo

JORGE MORA
Zenodo (CERN European Organization for Nuclear Research)
earthquake and tectonic studies
preprint

Timoshenko Flexocompression Beam Analogy Applied to the Calculation of Seismogenic Thickness and Cortical Rupture Prediction in the Sierra de Pie de Palo

JORGE MORA
preprint en

Abstract

This paper presents a deterministic geomechanical model to parameterize the spatial variabilityof seismogenic thickness (h) in basement thrust faults under flat-slab subduction regimes. We developa physico-mathematical analogy by transforming the elemental elastic approximation into avariable cross-section Timoshenko beam model subjected to tectonic flexocompression. The governingdifferential equations are solved numerically over a regularized mesh using interseismic strainrates derived from GPS data. The lower seismogenic boundary (zmax) is formulated by coupling theeffective stress tensor, deep dehydration-induced pore pressure, and rheological constitutive equations.The model is quantitatively calibrated and validated against hypocentral depths recorded byINPRES, and its integration into probabilistic seismic hazard assessment schemes is discussed

Zenodo (CERN European Organization for Nuclear Research)
National University of San Juan (AR)
Climate action
earthquake and tectonic studies
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