Comau Fjords coincide with the regional
trace of the Liquiñe-Ofqui Fault Zone, a
major NNE-striking, right-lateral strike-slip
structure that accommodates the parallel
regional (about 1,200 km long) structure of NNE trend that crosses
the Aysén Fjord (Cembrano and Hervé 1993; Fig. 1). Seismic activity
has been interpreted as partially related with magmatic activi...