Large deep-seated landslides occurred in Nara, Wakayama, and Mie prefectures
of western Japan when Typhoon Talas passed through the region on
September 3-4, 2011. Signals of large landslides have been recorded
by seismic networks around the world, and overall force estimates
have been previously determined for large landslides using long-period
waves. This study focuses on the high-frequency waveforms and presents
signals of 18 landslides caused by Typhoon Talas (2011). The location
of the landslides can be determined by a seismological back-projection
technique and these locations correlate with the observed surface
features. We have found that the volumes of the landslide correlated
with an energy parameter derived from the seismic records.
%0 Journal Article
%1 yamada_etal:2012
%A Yamada, Masumi
%A Matsushi, Yuki
%A Chigira, Masahiro
%A Mori, Jim
%D 2012
%J Geophysical Research Letters
%K geophysics seismology
%N 13
%P L13301+
%R 10.1029/2012GL052174
%T Seismic recordings of landslides caused by Typhoon Talas (2011),
Japan
%U http://dx.doi.org/10.1029/2012GL052174
%V 39
%X Large deep-seated landslides occurred in Nara, Wakayama, and Mie prefectures
of western Japan when Typhoon Talas passed through the region on
September 3-4, 2011. Signals of large landslides have been recorded
by seismic networks around the world, and overall force estimates
have been previously determined for large landslides using long-period
waves. This study focuses on the high-frequency waveforms and presents
signals of 18 landslides caused by Typhoon Talas (2011). The location
of the landslides can be determined by a seismological back-projection
technique and these locations correlate with the observed surface
features. We have found that the volumes of the landslide correlated
with an energy parameter derived from the seismic records.
@article{yamada_etal:2012,
abstract = {Large deep-seated landslides occurred in Nara, Wakayama, and Mie prefectures
of western Japan when Typhoon Talas passed through the region on
September 3-4, 2011. Signals of large landslides have been recorded
by seismic networks around the world, and overall force estimates
have been previously determined for large landslides using long-period
waves. This study focuses on the high-frequency waveforms and presents
signals of 18 landslides caused by Typhoon Talas (2011). The location
of the landslides can be determined by a seismological back-projection
technique and these locations correlate with the observed surface
features. We have found that the volumes of the landslide correlated
with an energy parameter derived from the seismic records.},
added-at = {2012-09-01T13:08:21.000+0200},
author = {Yamada, Masumi and Matsushi, Yuki and Chigira, Masahiro and Mori, Jim},
biburl = {https://www.bibsonomy.org/bibtex/290c1d331ab651deb2def5316e5d427aa/nilsma},
day = 7,
doi = {10.1029/2012GL052174},
interhash = {a5165f3c54a7d9682713cd27bf721084},
intrahash = {90c1d331ab651deb2def5316e5d427aa},
issn = {0094-8276},
journal = {Geophysical Research Letters},
keywords = {geophysics seismology},
month = jul,
number = 13,
pages = {L13301+},
timestamp = {2021-02-09T13:25:06.000+0100},
title = {Seismic recordings of landslides caused by Typhoon Talas (2011),
Japan},
url = {http://dx.doi.org/10.1029/2012GL052174},
volume = 39,
year = 2012
}