Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Kazuko Usami"'
Publikováno v:
Progress in Earth and Planetary Science, Vol 10, Iss 1, Pp 1-12 (2023)
Abstract Deep-sea turbidite has been used to determine the history of occurrence of large earthquakes. Surface-sediment remobilization is a mechanism of the generation of earthquake-induced turbidity currents. However, the detailed mechanism of surfa
Externí odkaz:
https://doaj.org/article/e4f1912ea39e462597f9e3db97ee9f32
Publikováno v:
Progress in Earth and Planetary Science, Vol 10, Iss 1, Pp 1-1 (2023)
Externí odkaz:
https://doaj.org/article/a7dec109d8f94e13bdd8ff4c79aee0e6
Autor:
Kan-Hsi Hsiung, Toshiya Kanamatsu, Ken Ikehara, Kazuko Usami, Chorng-Shern Horng, Naohiko Ohkouchi, Nanako O. Ogawa, Saneatsu Saito, Masafumi Murayama
Publikováno v:
Progress in Earth and Planetary Science, Vol 8, Iss 1, Pp 1-17 (2021)
Abstract The southwestern Ryukyu Trench represents the ultimate sink of sediments shed from Taiwan into the Philippine Sea, which are mainly transported to the trench by turbidity currents via submarine canyons. Here, we present trench turbidites int
Externí odkaz:
https://doaj.org/article/a61d64073dc64c459c5fa171b9f29d70
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Submarine canyons are efficient sediment transport pathways from shallow marine areas to deep sea. Along active margins, large tsunamis are a trigger for sediment transport to deep sea. However, sediment transport through submarine canyons by such ex
Externí odkaz:
https://doaj.org/article/7fb6a7abef5046f9a88f445f2a4e8fb7
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-9 (2020)
Abstract Deep-sea turbidites have been utilized to understand the history of past large earthquakes. Surface-sediment remobilization is considered to be a mechanism for the initiation of earthquake-induced turbidity currents, based on the studies on
Externí odkaz:
https://doaj.org/article/19a21c4b036f4ba580c5d0ba1184d84c
Publikováno v:
Geoscience Letters, Vol 5, Iss 1, Pp 1-12 (2018)
Abstract On the landward slope of the Japan Trench, the mid-slope terrace (MST) is located at a depth of 4000–6000 m. Two piston cores from the MST were analyzed to assess the applicability of the MST for turbidite paleoseismology and to find out r
Externí odkaz:
https://doaj.org/article/b4109f2701284d1d924927b7349f8105
Publikováno v:
Earth, Planets and Space, Vol 72, Iss 1, Pp 1-9 (2020)
Deep-sea turbidites have been utilized to understand the history of past large earthquakes. Surface-sediment remobilization is considered to be a mechanism for the initiation of earthquake-induced turbidity currents, based on the studies on the event
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5ec0de0ae8171c2a1e15a90c25e28350
http://link.springer.com/article/10.1186/s40623-020-01241-y
http://link.springer.com/article/10.1186/s40623-020-01241-y
Publikováno v:
Geological Society, London, Special Publications. 501:391-403
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b4a4cb1cce74a2c0a2270d9b5e8eb66
https://doi.org/10.1144/sp501-2019-53
https://doi.org/10.1144/sp501-2019-53
Autor:
Masafumi Murayama, Ken Ikehara, Kazuko Usami, Saneatsu Saito, Nanako O. Ogawa, Kan-Hsi Hsiung, Toshiya Kanamatsu, Naohiko Ohkouchi, Chorng-Shern Horng
Publikováno v:
Progress in Earth and Planetary Science, Vol 8, Iss 1, Pp 1-17 (2021)
The southwestern Ryukyu Trench represents the ultimate sink of sediments shed from Taiwan into the Philippine Sea, which are mainly transported to the trench by turbidity currents via submarine canyons. Here, we present trench turbidites intercalated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b61c16cbaa677a983cf4804d4b0c9ec4
https://doi.org/10.1186/s40645-020-00396-2
https://doi.org/10.1186/s40645-020-00396-2
Autor:
Arata Kioka, Tobias Schwestermann, Michael Strasser, Kazuko Usami, Ken Ikehara, Toshiya Kanamatsu
Publikováno v:
Understanding and Reducing Landslide Disaster Risk ISBN: 9783030601959
Sediment gravity flow is a density current that moves down a slope due to the gravitational force. Submarine landslides are a trigger mechanism for sediment gravity flows, and the movement of a large amount of sediment mass has the potential for gene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d143db295a9aa90223effb2c1395dbf
https://doi.org/10.1007/978-3-030-60196-6_26
https://doi.org/10.1007/978-3-030-60196-6_26
