Zobrazeno 1 - 10
of 100
pro vyhledávání: '"the 2018 Hokkaido Eastern Iburi earthquake"'
Publikováno v:
Earth, Planets and Space, Vol 75, Iss 1, Pp 1-14 (2023)
Abstract The Yufutsu Plain, a sedimentary basin surrounded by mountains, is located in the southern part of the Ishikari–Yufutsu Lowlands, Hokkaido, Japan. The Hidaka arc–arc collision zone, located in the eastern part of the Yufutsu Plain, forms
Externí odkaz:
https://doaj.org/article/5b0a7bc907774ea3b043635c08735078
Autor:
Jun Kameda
Publikováno v:
Earth, Planets and Space, Vol 74, Iss 1, Pp 1-12 (2022)
Abstract The 6.7 M w Eastern Iburi earthquake of 6 September 2018 triggered destructive landslides in southern Hokkaido, Japan, many of which were characterized by the flow-like downslope movement of volcanic soils formed from weathered tephra contai
Externí odkaz:
https://doaj.org/article/aa239bec1025465eb9b9a19119026a4f
Autor:
Jun Kameda
Publikováno v:
Progress in Earth and Planetary Science, Vol 8, Iss 1, Pp 1-13 (2021)
Abstract Destructive landslides were triggered by the 6.7 Mw Eastern Iburi earthquake that struck southern Hokkaido, Japan, on 6 September 2018. Heavy rainfall on 4 September in addition to intermittent rainfall around the Iburi Tobu area saturated a
Externí odkaz:
https://doaj.org/article/b88ae78d98e3426e9dbbb3e471c19834
Autor:
Jun Kameda, Atsushi Okamoto
Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-9 (2021)
Abstract Destructive landslides were triggered by the 6.7 M w Eastern Iburi earthquake that struck southern Hokkaido, Japan, on 6 September 2018. In this study, we carried out 1-D inversion analysis of one of the shallow landslides near the epicenter
Externí odkaz:
https://doaj.org/article/8fcff66cf3c24b3cb018eac77ed5dde4
Publikováno v:
Frontiers in Earth Science, Vol 9 (2022)
The earthquake that occurred on 6 September 2018, in the eastern part of the Iburi region of Hokkaido, Japan (the Hokkaido Eastern Iburi Earthquake) caused thousands of shallow landslides in mountain areas. In areas where many landslides occurred, th
Externí odkaz:
https://doaj.org/article/ef8b2fcea32f4593b70975d020a854ef
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-14 (2020)
Abstract The cloud-free, wide-swath, day-and-night observation capability of synthetic aperture radar (SAR) has an important role in rapid landslide monitoring to reduce economic and human losses. Although interferometric SAR (InSAR) analysis is wide
Externí odkaz:
https://doaj.org/article/f32b5a8d9a574b5dbce2fe077dfabd3f
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-11 (2020)
Abstract In this study, we investigate the source rupture process of the 2018 Hokkaido Eastern Iburi earthquake in Japan (M JMA 6.7) and how the ground motion can be reproduced using available source and velocity models. First, we conduct a multiple-
Externí odkaz:
https://doaj.org/article/74d90706afdc46fcba7e3468cb4de0e3
Autor:
Tomo Shibata, Ryo Takahashi, Hiroaki Takahashi, Takanori Kagoshima, Naoto Takahata, Yuji Sano, Daniele L. Pinti
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-8 (2020)
Abstract Six wells were continuously monitored in Hokkaido, northern Japan, to relate groundwater level changes to regional seismic activity. Groundwater level changes following the 2018 Hokkaido Eastern Iburi earthquake were detected in three of the
Externí odkaz:
https://doaj.org/article/5f354bf1f7b24ed28e6a80f098588646
Autor:
Ryoichi Nakamura, Takahiro Shiina
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-10 (2019)
Abstract We investigate S-wave attenuation (Qs) structure in and around Hokkaido, Japan, including the source area of the 2018 Hokkaido Eastern Iburi Earthquake (M 6.7) and its aftershocks. From the strong-motion seismograms recorded in the nationwid
Externí odkaz:
https://doaj.org/article/6a3f5319a12e4579886b51a47606f8db
Autor:
Kimiyuki Asano, Tomotaka Iwata
Publikováno v:
Earth, Planets and Space, Vol 71, Iss 1, Pp 1-17 (2019)
Abstract The source rupture process of the 2018 Hokkaido Eastern Iburi earthquake (M JMA 6.7) was analyzed by a kinematic waveform inversion method using strong-motion data in 0.04–0.5 Hz. This earthquake occurred close to the Hidaka Collision Zone
Externí odkaz:
https://doaj.org/article/1b0d6dc8e3f74f2e954746a7325e5a0f