Zobrazeno 1 - 10
of 63
pro vyhledávání: '"Hitoshi Onuki"'
Autor:
Makoto Inai, Masayoshi Mochizuki, Hitoshi Onuki, Takumi Furuta, Toshiyuki Wakimoto, Toshiyuki Kan, Mai Ito
Publikováno v:
Synlett. 2009:3373-3377
A concise solid-supported synthesis of artificial phospholipids was developed. Functionalized phospholipids were prepared by introduction of a head group onto a solid-supported phospholipid framework in good overall yield and purity.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28d181f48db52192f85079194d004d7d
https://doi.org/10.1055/s-0029-1218364
https://doi.org/10.1055/s-0029-1218364
Publikováno v:
JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY. 88:28-33
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9cd1e4004b096ebe7de986554825baea
https://doi.org/10.2465/ganko.88.28
https://doi.org/10.2465/ganko.88.28
Publikováno v:
JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY. 86:100-111
Two kinds of magma are probably derived from the initial magma in the Himekami pluton. The content of magnesium is the major difference between the two magmas. They produce the present four rock groups through two different processes in which the rat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c694c2f60652a5007b69dfa0c4f1b80
https://doi.org/10.2465/ganko.86.100
https://doi.org/10.2465/ganko.86.100
Autor:
Hitoshi Onuki, Tatuhiro Tanokura
Publikováno v:
JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY. 85:257-269
In the Hanaoka mining area of the “Green Tuff” region, the Miocene submarine lavas and pyroclastic rocks with basaltic to andesitic compositions were recrystallized at low temperatures to form various secondary minerals. The upper metabasites are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1bdc4f22de2c9632b6c9131f36df59f3
https://doi.org/10.2465/ganko.85.257
https://doi.org/10.2465/ganko.85.257
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 76:372-375
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::316afd598e650d5c7518d0dc322945e8
https://doi.org/10.2465/ganko1941.76.372
https://doi.org/10.2465/ganko1941.76.372
Autor:
Hitoshi Onuki, Michio Tagiri
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 71:229-237
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5c1efc05e622d12cc7b26415d6f845f
https://doi.org/10.2465/ganko1941.71.229
https://doi.org/10.2465/ganko1941.71.229
Autor:
Norihisa Ishimoto, Hitoshi Onuki
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 75:209-215
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ddc289a4a1f0943f5e0f5afc96fc7a9e
https://doi.org/10.2465/ganko1941.75.special2_209
https://doi.org/10.2465/ganko1941.75.special2_209
Publikováno v:
Memoirs of National Institute of Polar Research. Special issue. 14:153-163
Chemical compositions of biotites and hornblendes in metamorphic rocks around Lutzow-Holmbukta show that these minerals have the characteristics of granulite facies ones. Some low-Ti biotites and hornblendes may be due to low TiO_2 content of host ro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::64de847b7aa3e2db57a4f995fd2e890f
http://id.nii.ac.jp/1291/00001029/
http://id.nii.ac.jp/1291/00001029/
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 72:361-365
K-Ar ages were determined on some metamorphic rocks from the Sanbagawa terrain. The ages obtained are mostly of Middle and Late Cretaceous (110-67 m. y.). This range may not indicate the age of the main stage of metamorphism, but may represent the ag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::338633da5d1bdeb27885f12e88449e99
https://doi.org/10.2465/ganko1941.72.361
https://doi.org/10.2465/ganko1941.72.361
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 77:438-454
The Nishidohira cortlandtitic mass of probable Late Mesozoic age in the southern Abukuma Mountains has been characterized on the basis of field evidence, microscopic observations and chemical analyses of rocks and minerals. Though the mass is small,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff62a174ff9e2f8782a5ec737e976548
https://doi.org/10.2465/ganko1941.77.438
https://doi.org/10.2465/ganko1941.77.438