SciELO - Scientific Electronic Library Online

 
vol.11 número2ACURATE GRAVITY ANOMALY INTERPOLATION:: A CASE-STUDY IN CAMERRON, CENTRAL AFRICACLUSTERING ON DISSIMILARITY REPRESENTATIONS FOR DETECTING MISLABELLED SEISMIC SIGNALS AT NEVADO DEL RUIZ VOLCANO índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • En proceso de indezaciónCitado por Google
  • No hay articulos similaresSimilares en SciELO
  • En proceso de indezaciónSimilares en Google

Compartir


Earth Sciences Research Journal

versión impresa ISSN 1794-6190

Resumen

PEDRAZA GARCIA, Patricia; VARGAS, Carlos Alberto  y  MONSALVE J., Hugo. GEOMETRIC MODEL OF THE NAZCA PLATE SUBDUCTION IN SOUTHWEST COLOMBIA. Earth Sci. Res. J. [online]. 2007, vol.11, n.2, pp.124-134. ISSN 1794-6190.

A geometric model for the subduction of the Nazca plate beneath the South American plate in southwestern of Colombia is proposed based on the relocation of hypocenters of local and distant earthquakes. By means of the simultaneous inversion of teleseismic P and SH body waves, we constrained the depths of the 15 events with Mw ³ 5.8 and relocated the hypocenters of the 250 earthquakes recorded between 1990 and 2005 by: the International Seismological Centre (ISC) and U.S. Geological Survey, National Earthquake Information Center (NEIC) were relocated. A model is proposed for the hypocentral sections taking into account the trench along of the Earth and Colombia-Ecuador. We obtained three different possible shapes of subduction of the Nazca plate in the Colombia-Ecuador trench: The first configuration, in the Cali A segment, the dip angle changes from17º to 45º down to a maximum depth of 100km, the second configuration, in the Popayán B and Nariño C segments the dip angle holds approximately constant at 30º down to a maximum depth of 200 km and the third configuration, in the Quito D segment the dip angle changes of 9º to 50º to a maximum depth 220 km . The maximum depth of seismicity along the Colombia-Ecuador trench shows two increases, first between latitudes 4.5ºN-5ºN and second between the latitudes 1ºS-2ºS, suggesting that the presence of the Malpelo and Carnegie Ridges may generate a differential blockage at the Pacific Colombia-Ecuador basin.

Palabras clave : Seismotectonic; Nazca plate; subduction; Colombia.

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

 

Creative Commons License Todo el contenido de esta revista, excepto dónde está identificado, está bajo una Licencia Creative Commons