SciELO - Scientific Electronic Library Online

 
vol.73 número2Evidencias paleosísmica y arqueosísmica de la simbología Posclásica Tardía P'urhepecha en Michoacán (México). ¿Primeras señalizaciones sísmicas de la historia?Análisis de sismos interplaca, Pacífico central de Costa Rica: los sismos de Esterillos (13 de noviembre de 2017) y Herradura (24 de agosto de 2020) índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Boletín de la Sociedad Geológica Mexicana

versión impresa ISSN 1405-3322

Resumen

GINER-ROBLES, Jorge Luis et al. Strain 3D analysis and kinematics of the Middle American Trench in the junction of the Rivera and Cocos plates with the North-American and Caribbean plates. Bol. Soc. Geol. Mex [online]. 2021, vol.73, n.2, 00013.  Epub 31-Ene-2022. ISSN 1405-3322.  https://doi.org/10.18268/bsgm2021v73n2a150121.

In this work, we propose a kinematic model based on the strain 3D spatial distribution from focal mechanism solutions of instrumental earthquakes located along the Middle American Trench, in the convergence zone of Rivera and Cocos plates with North-American and Caribbean tectonic plates. We have used more than 1300focal mechanisms of' earthquakes (M ≥ 5.5), from the Global Centroid-Moment-Tensor (CMT) online global program to perform a cluster analysis of the spatial distribution of the tectonic strain tensor (ey, ex, ez) and its shape (k'). Accordingly, we have applied the Right Dihedral Method to a population of geographically clusteredfocal mechanisms, as well as the Slip Method, based on the slip data on the theoretical fault plane, for determining the extensional, compressive, and strike-slip zones, in correspondence with the principal tectonic features. Furthermore, we have realized 14 depth pro/files across the Middle American Trench (MAT) of the shape of the strain tensor and ternary Kaverina diagrams for constraining the tectonic deformation and developing a 3D model of the kinematics in the region. This analysis depicts a zonation in relation with the changing subduction angle of the slab and an increase of the convergence rate towards the SE, resulting from the mechanical coupling of the subduction, and showing less thrust earthquakes at the Rivera-North American convergence zone than at the Cocos-North American one. The proposed 3D geometry is in good agreement with the spatial distribution of large earthquakes, the slab dip angle, the presence of mantle currents at a 100 km depth and the occurrence of normal-type earthquakes. This model could also account for the presence of anomalous earthquakes such as slow and silent earthquakes in the Guerrero Gap.

Palabras llave : focal mechanism; Inversion; strain tensor; k'; Mexico.

        · resumen en Español     · texto en Español     · Español ( pdf )