Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Jun'ichi ITO"'
Autor:
Jun’ichi ITO
Publikováno v:
AIJ Journal of Technology and Design. 29:362-367
Autor:
Jun’ichi ITO
Publikováno v:
AIJ Journal of Technology and Design. 28:385-390
Autor:
Jun’ichi Ito
Publikováno v:
AIJ Journal of Technology and Design. 27:1384-1389
Autor:
Jun'ichi Ito
Publikováno v:
Journal of Architecture and Planning (Transactions of AIJ). 82:179-189
Autor:
Hiroaki Sato, Jun’ichi Ito, Xueyuan Yu, Hai-Xiang Zhang, Kentaro Terada, He-Cai Niu, Takashi Nagao, Qi Zhang
Publikováno v:
Journal of Asian Earth Sciences. 28:439-456
We present petrographic and geochemical data on representative samples of the Devonian adakite, boninite, low-TiO2 and high-TiO2 basalts and associated rocks in the southern Altay areas, Xinjiang, NW China. These volcanic rocks mostly occur as tecton
Autor:
Hiroaki Sato, Hai-Xiang Zhang, Boyou Zhang, He-Cai Niu, Qiang Shan, Takashi Nagao, Xueyuan Yu, Jun’ichi Ito
Publikováno v:
The Island Arc. 14:55-68
Volcanic rocks consisting of adakite and Nb-enriched basalt are found in the early Devonian Tuoranggekuduke Group in the northern margin of the Kazakhstan- Junggar Plate, northern Xinjiang, northwest China. The geochemical characteristics of the ande
Publikováno v:
Chinese Science Bulletin. 48:2231-2235
Field observation, petrological and geochemical characteristics of plagiogranite from Kuerti ophiolite indicate a similar origin to those in shearing zones. It is derived from partial melting of amphibolite that is developed from gabbro within the oc
Autor:
Jun'ichi Ito
Publikováno v:
The Journal of The Institute of Electrical Engineers of Japan. 122:374-377
Publikováno v:
Journal of Geography (Chigaku Zasshi). 109:774-783
Autor:
Jun'ichi Ito, Keiichi Shiraki
Publikováno v:
The Journal of the Geological Society of Japan. 105:810-813
Picrite basalts containing MgO up to 16 wt.% were found in the lowest part of the Pliocene Uegusukudake Formation on the north coast of Kumejima island ; in the close proximity northwest of the island lies an active back-arc basin, Okinawa Trough. Th