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The potential seismic hazard of the Tarímbaro-Álvaro Obregón fault, a major structure of the Morelia-Acambay fault system in central México

Author

Listed:
  • Martha Gabriela Gómez-Vasconcelos

    (Universidad Michoacana de San Nicolás de Hidalgo)

  • Denis Ramón Avellán

    (CONAHCYT-Instituto de Geofísica Unidad Michoacán, UNAM campus Morelia)

  • Jesús Avila García

    (Ciudad Universitaria)

  • Pierre Lacan

    (Universidad Nacional Autónoma de México)

  • Isabel Israde-Alcántara

    (Universidad Michoacana de San Nicolás de Hidalgo)

  • Oscar García

    (Xochipala Gold)

  • Jélime Aray Castellano

    (Universidad Nacional Autónoma de México)

  • Laurence Audin

    (Institut des Sciences de la Terre, ISTerre, IRD, Université Grenoble Alpes)

Abstract

Seismic hazard assessment in central México is essential considering the numerous crustal active faults crossing densely populated cities. The Morelia-Acambay Fault System in central México comprises at least thirty active E-W normal fault zones that affect Miocene to Holocene rocks and are responsible for several devastating earthquakes. However, most of these faults are unstudied; their behavior and seismogenic potential are unknown. The ENE-striking ~ 40-km-long Tarímbaro-Álvaro Obregón (TAO) fault is one of these major tectonic structures. It is located on the northern border of the Morelia Metropolitan area, where ca. one million inhabitants live within 10 km of the fault. We studied this normal fault through a detailed and multidisciplinary characterization due to its large surface expression and the current anthropization, which makes using classical techniques difficult. This study integrates geological, geophysical, and quantitative geomorphology, providing data for a better seismic hazard assessment. The TAO fault zone comprises three right-stepping en échelon segments separated by relay zones. This study reveals a mean vertical slip rate of 0.04 ± 0.08 mm/yr and 1.3 m of single-event vertical displacement. The TAO fault can produce earthquakes of magnitude 6.2 to 7.2, representing a significant potential seismic source in central México.

Suggested Citation

  • Martha Gabriela Gómez-Vasconcelos & Denis Ramón Avellán & Jesús Avila García & Pierre Lacan & Isabel Israde-Alcántara & Oscar García & Jélime Aray Castellano & Laurence Audin, 2025. "The potential seismic hazard of the Tarímbaro-Álvaro Obregón fault, a major structure of the Morelia-Acambay fault system in central México," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 121(1), pages 109-133, January.
  • Handle: RePEc:spr:nathaz:v:121:y:2025:i:1:d:10.1007_s11069-024-06832-6
    DOI: 10.1007/s11069-024-06832-6
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