Kyushu

N. Sakamoto and K. Moriaaga Sogo Rikogaku Hokoku (Kyushu Daigaku Daigakuin) 12(3), 283—289 (1990). 

Institute of Advanced Material Study Kyushu University, Kasugakoen Kasuga 816-8580 Japan... 

K. Yanagawa, S. Nagai, M. Shimada, and A. Ueda, Preprints of 32nd Joint Meeting, Kyushu Sections of Chemistry Related Societies, Japan, p. 127 (Fukuoka, 1995). 

Yamagata K, Hironai E, Mishikawa K, Matsouka H (1955) Nucleate boihng of water on the horizontal heating surface. Memoirs of the Eaculty of Engineering, vol 15. Kyushu University, Japan, p 98... 

Conjugate Additions Sogo Rikogaku Kenkyuka Hokoku (Kyushu Daigaku Daiga-kuin) 1995 17 353-359... 

Hayashida, T Nagashima, H. Reports Inst. Adv. Mater Study (Kyushu Univ.) 2001, 15, 31. 

Department of Organic Synthesis Kyushu University Hakozaki 6-10-1, Higashi-ku Fukuoka 812, Japan... 

The research work described here was carried out by an able group of students of Yamaguchi University and Ube Techinical College, and in collaboration with our laboratory staffs and industrial colleagues. In particular, Dr. S. Fujisaki and Dr. T. Okamoto made significant contributions. We thank them all, and also Dr. H. Tsuzuki of Central Analytical Center of Kyushu University undertook X-ray crystal structure analysis of BTMA Br3. Furthermore, we wish to thank Professor M. Tashiro of Kyushu University for useful discussions. Finally, we are grateful to Professor Y. Sasson of The Hebrew University of Jerusalem, Chairman of the Scientific Committee of Orgabrom 93, for the invitation to present this work in Jerusalem. 

S. Kajigaeshi, T. Kakinami, M. Moriwaki, S. Fujisaki, M. Tashiro, Rep. Inst. Advanced Material Study, Kyushu Univ., 2, 87 (1988). 

N. Tamari, Y. Otsubo, A. Kato, Kyushu Daigaku Kogaku Shuno, 49, 531 (1976) Chem. Abstr., 86, 59,469p (1977). 

T. Watanabe, in Proceedings of the 4th International Conference on High Pressure, Kyoto, 1974, p. 138 Chem. Ahstr., 83, 83,912m (1975) Kyushu Kogyo Gijutsu Shikensho Hokoku, 21, 1238 (1978) Chem. Ahstr., 91, 43,053r (1979). 

Institute for Materials Chemistry and Engineering Kyushu University Fukuoka, Japan... 

Katsuki T, Watanabe A, Uchida T (2003) EP 1352908. To Kyushu University Watanabe A, Ushida T, Katsuji I, Katsuki T (2002) Tetrahedron Lett 43 4481 Shargi H, Eskandari MM (2003) Tetrahedron 59 8509 Zhang TY, Allen MJ (1999) Tetrahedron Lett 40 5813... 

Graduate School of Engineering Sciences, Kyushu University 6-1 Kasugakoen, Kasuga, Fukuoka 816 Japan... 

FIGURE 25.5 Arrhenius plots of some oxide ion conductors. (Courtesy of Prof. Tatsumi Ishihara, Kyushu University, Japan.)... 

The author is grateful to Mr. H. Horiuchi for the preparation of photoelectrochemical cells. Professor S. Yamada for discussion, and Professor Y. Tanimoto and Associate Professor Y. Fujiwara for using the superconducting magnets. The author also thanks The Center of Advanced Instrumental Analysis, Kyushu University, for H-NMR measurements. This study was financially supported by the Grant-in-Aids for Scientific Research Priority Areas (Area 767, No. 15085203) and (Area 432, No. 17034051), Scientific Research (C) (No. 17550131), and twenty first century COE Program Function Innovation of Molecular Informatics from M EXTof the Japan. 

Masahiro Irie received his B.S. and M.S. degrees from Kyoto University and his Ph.D. in radiation chemistry from Osaka University. He joined Hokkaido University as a research associate in 1968 and started his research on photochemistry. In 1973 he moved to Osaka University and developed various types of photoresponsive polymers. In 1988 he was appointed Professor at Kyushu University. In the middle of the 1980 s he invented a new class of photochromic molecules - diaryl-ethenes - which undergo thermally irreversible and fatigue resistant photochromic reactions. He is currently interested in developing singlecrystalline photochromism of the diarylethene derivatives. 

Kyushu University Eaculty of Engineering Department of Chemical Engineering Moto-Oka, Nishi Ku Eukuoka 819-0395 Japan... 

Kyushu University Department of Applied Chemistry 6-10-1 Hakozaki, Higashi-ku Fukuoka 812-8581 Japan... 

Taura F, Morimoto S, Shoyama Y (1996) J Biol Chem 271 17411 Morimoto S, Komatsu K, Taura F, Shoyama Y (1998) Phytochemistry 49 1525 Taura F, Morimoto S, Shoyama Y, Mechoulam R (1995) J Am Chem Soc 117 9766 Taura U (2004) Research report, Graduate School of Pharmceutical Sciences, Kyushu University. Available at http //www.nisr.or.jp/englishHP/report2004/NlSR04tam-a.pdf, last visited 29 June 2007... 

The coupled precipitation kinetics-fluid flow model was applied to the distribution of Si02 content and K2O content of the hydrothermally altered andesite in the Hishikari Au-Ag mine area, south Kyushu, Japan by Shikazono et al. (2002). This will be described in section 1.4.6. 

S C and 8 0 of carbonates from southern Kyushu (Hokusatsu gold district) have been studied in detail (Matsuhisa et al., 1985 Morishita, 1993). Morishita (1993) found that the S C values of hydrothermal solution in the district during the mineralization stages were low (—ll%c), compared with that of average crustal carbon (—7%o), suggesting that of hydrothermal solution is controlled by organic carbon in widely distributed sedimentay rocks of the Cretaceous Shimanto Supergroup basement. 

Figure 1.114 demonstrates that the deposits in northeastern Hokkaido, central Honshu, Sado Island and Kyushu deposits are Non-Green tuff type and those in southwestern Hokkaido, Northeast Japan (Tohoku), the Izu Peninsula, and San-in are Green tuff-type. 

Sedimentary rocks often occur as host rocks, footwall rocks and basement rocks in the Non-Green tuff mine area. For example, in southern Kyushu, the Shimanto Supergroup shale is dominant as basement and a host rock for epithermal Au-Ag vein-type deposits (e.g., Hishikari). 

S S value of sedimentary rocks of the Shimanto Supergroup which hosts the Hishikari deposits, southern Kyushu is — 12%o (Ishihara et al., 1986) which is considerably lower than those of the Hishikari deposits (+l%o to - -2%c) (Shikazono, unpublished. This suggests that sedimentary sulfide sulfur is one of the sources of the sulfides and probably igneous sulfide sulfur is the dominant source. 

Morishita (1993) showed based on carbon isotopic composition of carbonates that carbon of carbonates in the gold-bearing quartz vein in southern Kyushu was derived from the Shimanto Supergroup shale. Imai et al. (1998) considered that hydrogen in the ore fluids was derived from the Shimanto Supergroup shale based on 5D (—60%o to — 100%c) of inclusion fluids in quartz and adularia of the Hishikari veins. These isotopic... 

As shown in Fig. 1.117, Se-type and Te-type epithermal Au-Ag vein-type deposits are located in the Cretaceous-Quaternary volcanic terrane of Japan (e.g., northeast and southwest Hokkaido, middle Honshu, south Kyushu). Some Te-type deposits are located in regions similar to the Se-type deposits. Sometimes, Te mineralization is associated with the Se-type deposits, though Te minerals usually do not coexist with Se minerals. However, rarely, Te minerals coexist with Se minerals in the Te-type deposits (e.g., Teine, Suzaki, Kawazu, Iriki) on a polished section scale. For example, coexistence of native Te and Se-bearing tetrahedrite is found at Teine. Generally, Te mineralization occurs at... 

This type of mixing could reasonably explain the occurrence of acidic alteration minerals such as kaolinite and alunite in the low-sulfidation epithermal gold vein district (e.g., Seta in northeast Hokkaido, Hishikari in southern Kyushu) (Yajima et al., 1997)... 

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