Zobrazeno 1 - 10
of 30
pro vyhledávání: '"Tadahide Ui"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 110, Iss 110, Pp 1-1 (1990)
Doğu ve Güneydoğu Anadolu'da Orta Miyosenden itibaren etkin olmaya başlayan çarpışma zonu volkanizması incelenmiş ve çeşitli yörelerdeki değişik yüzleklerinden örnekler alınarak majör, iz ve nadir toprak element (REE) kimyasal anali
Externí odkaz:
https://doaj.org/article/8655521c11214122acdca5be79a7d6bd
Autor:
Tadahide Ui, Toshitsugu Fujii, Takahiro Yamamoto, Shinji Takarada, Hiroaki Sato, Keiichi Sakaguchi, Shigeru Suto
Publikováno v:
Journal of Volcanology and Geothermal Research. 420:107343
This discussion concerns the flowage of the 1991 lava lobes at Unzen that were suggested by Goto et al. (2020) to be moving rigidly. Pictorial evidence of flowage of the 1991 lava lobe of Unzen, such as morphological change of the lava lobe, protrusi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f3d2bda067f923bfe244fbea636fdf4a
https://doi.org/10.1016/j.jvolgeores.2021.107343
https://doi.org/10.1016/j.jvolgeores.2021.107343
Autor:
Tadahide Ui
Publikováno v:
The Quaternary Research (Daiyonki-Kenkyu). 56:243-244
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c78087009485b1a08ae06f644de55a3
https://doi.org/10.4116/jaqua.56.243
https://doi.org/10.4116/jaqua.56.243
Publikováno v:
Journal of Volcanology and Geothermal Research. 152:1-19
The eruptive history of Fuji volcano has been dominated by basaltic volcanism. However, the 1707 eruption of Fuji volcano resulted in a chemically zoned pyroclastic deposit ranging from basalt to dacite. The processes responsible for generating these
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7119244303e53b868489505d0602489
https://doi.org/10.1016/j.jvolgeores.2005.08.002
https://doi.org/10.1016/j.jvolgeores.2005.08.002
Autor:
Tadahide Ui
Publikováno v:
Journal of Geography (Chigaku Zasshi). 110:285-288
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb9d00e38c36d26c80f10f4109ea1245
https://doi.org/10.5026/jgeography.110.2_285
https://doi.org/10.5026/jgeography.110.2_285
Publikováno v:
Geology. 28:1079-1082
Submersible observations and samples show that the lower south flank of Hawaii, offshore from Kilauea volcano and the active Hilina slump system, consists entirely of compositionally diverse volcaniclastic rocks; pillow lavas are confined to shallow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bd688ed5b29c8242169ddbed6c63b3cb
https://doi.org/10.1130/0091-7613(2000)028<1079:isoakv>2.3.co
https://doi.org/10.1130/0091-7613(2000)028<1079:isoakv>2.3.co
Publikováno v:
Bulletin of Volcanology. 60:508-522
The depositional features of two valley-filling debris avalanche deposits were studied to reveal their transportation and depositional mechanisms. The valley-filling Iwasegawa debris avalanche deposit (ca. 0.1 km3) is distributed along the valleys at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e079519f012f934202cc67d6a9d3948
https://doi.org/10.1007/s004450050248
https://doi.org/10.1007/s004450050248
Publikováno v:
Journal of Volcanology and Geothermal Research. 64:171-191
In central and eastern Anatolia, volcanism related to continental collision occurred in Neogene to Quaternary times. Major-and trace-element compositions,87Sr86/Sr and K-Ar ages were determined for volcanic rocks from selected volcanoes in this regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2f86fd4f07ff234f6274a844d0c0991
https://doi.org/10.1016/0377-0273(94)00077-t
https://doi.org/10.1016/0377-0273(94)00077-t
Publikováno v:
Hawaiian Volcanoes: Deep Underwater Perspectives
Joint Japan-USA cruises in 1998-99 explored and sampled the previously unstudied deep offshore region south of Kilauea. Bathymetric features, dive observations, and recovered samples indicate that the 3-km-deep mid-slope bench, bounded seaward by a 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1959ec29293d316f6fc77a8c156ceaca
https://doi.org/10.1029/gm128p0161
https://doi.org/10.1029/gm128p0161
Autor:
Jiro Naka, Nohiro Tsuboyama, Toshiya Kanamatsu, Thomas W. Sisson, Peter W. Lipman, John R. Smith, Julia K. Morgan, Tadahide Ui
Publikováno v:
Hawaiian Volcanoes: Deep Underwater Perspectives
Most slopes of the Hilina slump are steep, but local small benches, mantled by volcaniclastic sand and fine sediments, were sampled in 1998-1999 with ROV KAIKO and DSRV SHINKAI 6500. Most surficial glass sands on the Hilina slump have compositions of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5daed8599dd6660bff40801bec46118c
https://doi.org/10.1029/gm128p0029
https://doi.org/10.1029/gm128p0029