CRUSTAL VELOCITY MODELS OF SHEAR WAVES IN EAST ANTARCTICA BY RECEIVER FUNCTION INVERSION OF BROADBAND WAVEFORMS
P(論文) 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 reco...
Main Authors: | , , , , , |
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Language: | English |
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National Institute of Polar Research
1996
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Online Access: | https://nipr.repo.nii.ac.jp/record/2819/files/KJ00002409866.pdf https://doi.org/10.15094/00002819 https://nipr.repo.nii.ac.jp/records/2819 |