سال انتشار: ۱۳۹۰

محل انتشار: ششمین کنفرانس بین المللی زلزله شناسی و مهندسی زلزله

تعداد صفحات: ۸

نویسنده(ها):

F Sodoudi – GFZ Research Center for Geosciences, Telegrafenberg 4473 Potsdam, Germany
R Kind – GFZ Research Center for Geosciences, Telegrafenberg 4473 Potsdam, Germany
G Asch – GFZ Research Center for Geosciences, Telegrafenberg 4473 Potsdam, Germany

چکیده:

results obtained from S and P receiver functions produced a clear image of the top and bottom of the subducting nazca lithosphere beneath northern chile . Using data from the teleseismic events recorded at 15 permanent IPOC integrated plate boundary observatory chile stations we obtained new constraints on the geometry and thickness of the descending nazca lithosphere.