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Hokkaido University Collection of Scholarly and Academic Papers >
Showing results 1 to 8 of 8
Showing results 1 to 8 of 8
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Recent SubmissionsTakahata, Hiroyuki... [et al.] (1985) Dumortierite-Bearing Argillaceous Gneisses from the Abukuma Metamorphic Terrain, Northeast Japan. 北海道大学理学部紀要, 21(3): 465-481 Newly found dumortierite occurring as a minor constituent mineral in argillaceous gneisses of the Ab....
Johnson, Kevin T.M. (1985) Major, Trace, and Rare Earth Element Abudances in Boninitic Lavas from the Ogasawara Forearc. 北海道大学理学部紀要, 21(3): 453-463 Dredged andesites and dacites from the Ogasawara forearc contain high abundances of MgO at high SiO2....
Irifune, Tetsuo (1985) Experimental Study of the System Mg3Al2Si3O12-Mg3Cr2Si3O12 at High Pressure and High Temperature. 北海道大学理学部紀要, 21(3): 417-451 Phase relation between pyrope Mg3Al2Si3O12 and knorringite Mg3Cr2Si3O12 is determined experimentally....
Okamura, Satoshi (1985) Trace Element Abundances of the Late Tertiary Volcanic Rocks in Southwest Hokkaido. 北海道大学理学部紀要, 21(3): 405-416 Abundances of trace elements including REE were determined for 22 Late Tertiary (Late Miocene to Pli....
Bamba, Takeo (1985) Implication of the Composite Mineralization on the Massive Sulfide Deposits of the Shimokawa Mine. 北海道大学理学部紀要, 21(3): 363-404 Study on massive sulfide ores of the Shimokawa mine disclosed that the ores have been created by two....
Katsui, Yoshio... [et al.] (1985) Development of Faults and Growth of Usu-Shinzan Cryptodome in 1977-1982 at Usu Volcano, North Japan. 北海道大学理学部紀要, 21(3): 339-362 Usu-Shinzan, a cryptodome uplifted about 180 m, was built on the summit of Usu Volcano during the 19....
Tsuchiya, Nobutaka (1985) Fe-Ti Oxide Minerals in the Matsumae Plutonic Rocks, Southwestern Hokkaido, Japan. 北海道大学理学部紀要, 21(3): 321-337 The Matsumae plutonic rocks, consisting of ultramafic cumulates to adamellite, are divided into thre....
Igarashi, Toshihiko... [et al.] (1985) The Takadomari Serpentinites in the Kamuikotan Ophiolite Belt, Hokkaido, Japan. 北海道大学理学部紀要, 21(3): 305-319 Within the Kamuikotan Ophiolite Belt, a large serpentinite mass more than 10×12 km is observed aroun....
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