@article{10272/12652,
year = {1996},
url = {http://hdl.handle.net/10272/12652},
abstract = {The Chilean convergent margin south of the strait of Magellan represents an excellent opportunity to study a style of subduction where most of the parameters controlling this process remain approximately constant except one: obliquity. Modelling of Free Air anomaly data constrained with seismic data along a track perpendicular to the margin shows a well developed bathymetric terrace (Fuegian terrace) with a pronounced negative gravity anomaly, a common feature of active trenches, and a gently dipping (8U) slab subducting beneath the Scotia plate},
publisher = {Sociedad Geológica de España},
title = {Modelización de la estructura litosférica del margen Sur Chileno a partir de datos gravimétricos y sísmicos},
title = {Lithosferic structure of the Southernmost Chilean margin. Insights from gravity and seismic data},
author = {Rubio, E. and Torné, M. and Vera, E.},
}