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Multichannel Seismic Imaging of the Rivera Plate Subduction at the Seismogenic Jalisco Block Area (Western Mexican Margin)

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Geodynamics of the Latin American Pacific Margin

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Abstract

During the TSUJAL marine geophysical survey, conducted in February and March 2014, Spanish, Mexican and British scientists and technicians explored the western margin of Mexico, considered one of the most active seismic zones in America. This work aims to characterize the internal structure of the subduction zone of the Rivera plate beneath the North American plate in the offshore part of the Jalisco Block, to link the geodynamic and the recent tectonic deformation occurring there with the possible generation of tsunamis and earthquakes. For this purpose, it has been carried out acquisition, processing and geological interpretation of a multichannel seismic reflection profile running perpendicular to the margin. Crustal images show an oceanic domain, dominated by subduction–accretion along the lower slope of the margin with a subparallel sediment thickness of up to 1.6 s two-way travel time (approx. 2 km) in the Middle American Trench. Further, from these data the region appears to be prone to giant earthquake production. The top of the oceanic crust (intraplate reflector) is very well imaged. It is almost continuous along the profile with a gentle dip (<10°); however, it is disrupted by normal faulting resulting from the bending of the plate during subduction. The continental crust presents a well-developed accretionary prism consisting of highly deformed sediments with prominent slumping towards the trench that may be the result of past tsunamis. Also, a bottom simulating reflector (BSR) is identified in the first half a second (twtt) of the section. High amplitude reflections at around 7–8 s twtt clearly image a discontinuous Moho, defining a very gentle dipping subduction plane.

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  1. Estefanía Górriz

    Present address: Unidad de Tecnología Marina-CSIC, P. Marítimo de la Barceloneta 37-49, 08003, Barcelona, Spain

Authors and Affiliations

  1. Instituto de Ciencias del Mar-CSIC, P. Marítimo de la Barceloneta 37-49, 08003, Barcelona, Spain

    Rafael Bartolome, Estefanía Górriz & Alejandra L. Cameselle

  2. Unidad de Tecnología Marina-CSIC, P. Marítimo de la Barceloneta 37-49, 08003, Barcelona, Spain

    Juanjo Dañobeitia, Arturo Castellón & Jose Luis Alonso

  3. Universidad Complutense de Madrid, Ciudad Universitaria, Plaza Ciencias, s/n, 28040, Madrid, Spain

    Diego Cordoba

  4. Instituto de Ciencias de la Tierra Jaume Almera, C/Lluis Solé Sabaris s/n, 08028, Barcelona, Spain

    David Martí

  5. Centro Universitario de la Costa (CUC), Av. Universidad 203, Del. Ixtapa, 48280, Puerto Vallarta, Mexico

    Francisco Núñez-Cornú & Diana Nuñez

  6. Instituto de Geofísica, UNAM, Ciudad Universitaria, Delegación Coyoacán, C.P. 04510, México, DF, Mexico

    William L. Bandy & Carlos A. Mortera-Gutiérrez

  7. University of Barcelona, Marti i Franques s/n, 08028, Barcelona, Spain

    Estefanía Górriz

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Editors and Affiliations

  1. Instituto de Geofísica Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, 04510, Mexico, DF, Mexico

    William L. Bandy

  2. Vatican City State Holy See, Italy

    Juanjo Dañobeitia

  3. Instituto de Geofisica Universidad Nacional Autónoma de México, 04510, Mexico, Mexico

    Carlos Gutiérrez

  4. Volcanology Department, Institute of Geophysics, UNAM, 3000 Av. Universidad, 04510, Mexico, D.F., Mexico

    Yuri Taran

  5. Instituto de Ciencias del Mar-CSIC, P. Marítimo de la, Barceloneta 37-49, 08003, Barcelona, Spain

    Rafael Bartolomé

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Bartolome, R. et al. (2016). Multichannel Seismic Imaging of the Rivera Plate Subduction at the Seismogenic Jalisco Block Area (Western Mexican Margin). In: Bandy, W.L., Dañobeitia, J., Gutiérrez, C., Taran, Y., Bartolomé, R. (eds) Geodynamics of the Latin American Pacific Margin. Pageoph Topical Volumes. Birkhäuser, Cham. https://doi.org/10.1007/978-3-319-51529-8_19

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