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...
Published in: | Geophysical Journal International |
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Main Authors: | , , , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
2012
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/191/3/932 https://doi.org/10.1111/j.1365-246X.2012.05684.x |