P-wave velocity structure of the ice sheet and the shallow crust beneath the Mizuho traverse route, East Antarctica, from seismic refraction analysis

A seismic survey with a high density network was conducted by the 41st Japanese Antarctic Research Expedition (JARE-41) in the austral summer of 1999-2000. The seismic line was 190 km long, along the Mizuho traverse route from the base camp S16. 160 temporary seismic stations using data loggers were...

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Bibliographic Details
Main Authors: Tomoki Tsutsui, Hiroshi Murakami, Hiroki Miyamachi, Shigeru Toda, Masaki Kanao
Format: Report
Language:English
Published: Faculty of Engineering and Resource Science, Akita University/Technical Center for Seismological Observations/Faculty of Science, Kagoshima University/Faculty of Education, Aichi University of Education/National Institute of Polar Research 2001
Subjects:
seismic survey
Mizuho traverse route
Enderby Land
ice-sheet thickness
top crust
Antarctic
East Antarctica
Austral
Mizuho
Antarc*
Antarctica
Ice Sheet
Polar geoscience
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3094
http://id.nii.ac.jp/1291/00003094/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3094&item_no=1&attribute_id=18&file_no=1

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