Cinemática neotectónica de Cuba oriental

  1. M.O. Cotilla Rodríguez 1
  2. P. Bankwitz 2
  3. J.L. Alvarez Gómez 3
  4. H.J. Franzke 4
  5. M.F. Rubio Sauvalle 5
  6. J. Pilarski 2
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  2. 2 Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences
    info

    Helmholtz Centre Potsdam - GFZ German Research Centre for Geosciences

    Potsdam, Alemania

    ROR https://ror.org/04z8jg394

  3. 3 Centro Nacional de Investigaciones Sismológicas, Cuba
  4. 4 Clausthal University of Technology
    info

    Clausthal University of Technology

    Clausthal-Zellerfeld, Alemania

    ROR https://ror.org/04qb8nc58

  5. 5 Instituto de Geofísica y Astronomía
    info

    Instituto de Geofísica y Astronomía

    La Habana, Cuba

    ROR https://ror.org/05e5m0q38

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Revue:
Revista de la Sociedad Geológica de España

ISSN: 0214-2708

Année de publication: 1998

Volumen: 11

Número: 1-2

Pages: 33-42

Type: Article

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D'autres publications dans: Revista de la Sociedad Geológica de España

Résumé

The temporal - spatial location of Cuba at the meridional boundary of the North American Lithospheric Plate in direct relation with the smaller Caribbean Plate is responsible for the seismicity and neofaulting of the Eastern Neotectonic Unit. A kinematic of blocks model is proposed (three dynamic cells), which includes the action of vertical and horizontal neotectonic processes. The spatial arrangement of the cells allow us to explain the occurrence of earthquakes in the area and points out the differentiation of activity of the seismogenetic faults and knots.

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