P-wave velocity structure beneath the northern Antarctic Peninsula: evidence of a steeply subducting slab and a deep-rooted low-velocity anomaly beneath the central Bransfield Basin

Upper-mantle structure between 100 and 300 km depth below the northern Antarctic Peninsula is imaged by modelling P -wave traveltime residuals from teleseismic events recorded on the King Sejong Station (KSJ), the Argentinean/Italian stations (JUBA and ESPZ), an IRIS/GSN Station (PMSA) and the Seism...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Park, Yongcheol, Kim, Kwang-Hee, Lee, Joohan, Yoo, Hyun Jae, Plasencia L., Milton P.
Format: Text
Language:English
Published: Oxford University Press 2012
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/191/3/932
https://doi.org/10.1111/j.1365-246X.2012.05684.x