SHEAR WAVE VELOCITY STRUCTURE IN THE CRUST AND UPPERMOST MANTLE BENEATH SYOWA STATION, EAST ANTARCTICA, USING MULTI-TRACE RECEIVER FUNCTION INVERSION OF BROAD-BAND TELESEISMIC WAVEFORMS

• Main Authors: カナオ マサキ, シブタニ タクオ, Masaki KANAO, Takuo SHIBUTANI
• Format: Report
• Language: English
• Published: National Institute of Polar Research 1995
• Subjects: East Antarctica; Syowa Station; Mizuho; Mizuho Plateau; Antarc*; Antarctica; Enderby Land
• Online Access: https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2805; http://id.nii.ac.jp/1291/00002805/; https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2805&item_no=1&attribute_id=18&file_no=1

Receiver functions developed from teleseismic P-waveforms recorded on the broadband seismographs of Streckeisen seismometer (STS) at Syowa Station (69.0°S, 39.6°E), Enderby Land, Antarctica were inverted for vertical shear wave velocity structure beneath the station. By applying the source-equalizat...