CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS
Receiver functions from teleseismic earthquakes recorded with broadband seismographs at Dumont d'Urville Station (66.7°S, 140.0°E; DRV) and Mawson Station (67.6°S, 62.9°E; MAW), East Antarctica, are inverted for shear wave velocity models of the crust and uppermost mantle beneath the recording...
Main Authors: | , , , , , |
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Format: | Report |
Language: | English |
Published: |
National Institute of Polar Research
1996
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2819 http://id.nii.ac.jp/1291/00002819/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2819&item_no=1&attribute_id=18&file_no=1 |