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Author Nishiyama, Yoshihiro|
Published Date 2004-7
Publication Title Physical Review E
Volume volume70
Issue issue1
Content Type Journal Article
Author Takahashi, Norio| Miyabara, Shun-ichi| Fujiwara, Koji|
Published Date 1999-5
Publication Title Magnetics
Volume volume35
Issue issue3
Content Type Journal Article
Author Takahashi, Norio| Nakata, Takayoshi| Morishige, H.|
Published Date 1994-9
Publication Title Magnetics
Volume volume30
Issue issue5
Content Type Journal Article
Author Nakata, Takayoshi| Fujiwara, K.| Takahashi, N.| Nakano, Masanori| Okamoto, N.|
Published Date 1994-9
Publication Title Magnetics
Volume volume30
Issue issue5
Content Type Journal Article
Author Gotoh, Yuji| Takahashi, Norio|
Published Date 2002-3
Publication Title Magnetics
Volume volume38
Issue issue2
Content Type Journal Article
Author Nakata, Takayoshi| Takahashi, N.| Fujiwara, K.| Nakano, Masanori|
Published Date 1993-11-01
Publication Title Magnetics
Volume volume29
Issue issue6
Content Type Journal Article
Author Nakata, Takayoshi| Takahashi, N.| Fujiwara, K.|
Published Date 1990-3
Publication Title Magnetics
Volume volume26
Issue issue2
Content Type Journal Article
Author Ohnishi, Takuma| Takahashi, N.|
Published Date 2000-09-01
Publication Title Magnetics
Volume volume36
Issue issue5
Content Type Journal Article
Author Tsuboi, H.| Tanaka, H.| Fujita, M.|
Published Date 1989-9
Publication Title Magnetics
Volume volume25
Issue issue5
Content Type Journal Article
Author Nakata, Takayoshi| Takahashi, N.|
Published Date 1982-11
Publication Title Magnetics
Volume volume18
Issue issue6
Content Type Journal Article
Author Nakata, Takayoshi| Takahashi, N.|
Published Date 1982-3
Publication Title Magnetics
Volume volume18
Issue issue2
Content Type Journal Article
Author Ohnishi, Takuma| Takahashi, N.|
Published Date 2000-12-14
Publication Title Magnetics
Volume volume36
Issue issue5
Content Type Journal Article
Author Sano, Tetsuya| Yamamoto, Hideki|
Published Date 2002-5
Publication Title Instrumentation and Measurement Technology Conference
Volume volume1
Content Type Journal Article
Author Sano, Tetsuya| Yamamoto, Hideki|
Published Date 2001-5
Publication Title Instrumentation and Measurement Technology Conference
Volume volume1
Content Type Journal Article
Author Noritsugu, Toshiro| Tanaka, Toshihiro| Yamanaka, Takashi|
Published Date 1996-11
Publication Title Robot and Human Communication
Content Type Journal Article
Author Mukaigawa, Yasuhiro| Genda, Daisuke| Yamane, Ryo| Shakunaga, Takeshi|
Published Date 2003-8
Publication Title Multisensor Fusion and Integration for Intelligent Systems
Content Type Journal Article
Author Inoue, Akira| Deng, Mingcong| Harada, Takafumi| Baba, Yusuke| Morioka, Nobuhide| Mutou, Akinori| Ueki, Nobuyuki|
Published Date 2006-6
Publication Title Intelligent Control and Automation
Volume volume1
Content Type Journal Article
Author Tanaka, Yutaka| Gofuku, Akio| Nakamura, Keiji|
Published Date 1997-09-23
Publication Title Mechatronics and Machine Vision in Practice
Content Type Journal Article
Author Kamon, Yuji| Yamane, Ryo| Mukaigawa, Yasuhiro| Shakunaga, Takeshi|
Published Date 2005-6
Publication Title Proceedings of the Fifth International Conference on 3-D Digital Imaging and Modeling
Content Type Conference Paper
JaLCDOI 10.18926/21334
Title Alternative The Geochemistry of Rocks from Asama Volcano, Japan. New Approaches in the Quantitative Interpretation of the Chemical Composition of Volcanic Rocks
FullText URL pitsr_032_001_085.pdf
Author Matsui, Yoshito|
Abstract In dealing with the geochemistry of volcanic rocks, it appears imperative, first, to refine the procedure of rock analysis with respect to both major and minor components, and second, to improve present methods of interpreting analytical data on common rock suites such as basalts, andesites and dacites. In regard to the first problem, the rapid method of silicate analysis as described by Shapiro and Brannock (1956) and by Riley (1958) deserves special attention. With such a method it is possible to estimate the accuracy and precision of data with far greater ease than is possible with a classical one, yet without any loss of quality. For the determination of some components, however, it is felt that the procedures recommended previously lack precision and/or simplicity. In Part I of this paper, new methods are suggested for these components. The sum of Mg, Ca and Mn is titrated with EDTA in the presence of Al, Fe and other metals, using thymolphthalein complexone as indicator at pH 10-10.5. The sum of Al and Fe is determined by the back-titration of excess EDTA with the standard Cu solution. PAN is used as indicator at pH about 4, and tartrate is added as the masking agent of Ti. Na and K are determined by flame photometry using very dilute solutions (1-5ppm Na or K), without the separation of other metals and without the use of the internal standard. Sr is included in the scheme of analysis, and is determined by flame photometry according to the standard addition technique. These procedures are tested for their accuracy using the standard samples G-1 and W-1 (Tables 3, 5, 9, 12 and 15). Procedures for other components are also described in the text in full detail. The system of analytical procedures recommended is shown in Table 16. To investigate the problem of the interpretation of compositional variation, typical rocks from Asama volcano and the surrounding area were selected, namely, andesites and dacites of calc-alkaline type. Twenty-one samples, described in Tables 18 and 19, are analyzed according to the above procedures. Results are shown in Table 20. Variation diagrams are presented in Figs. 3 to 5. Since it may be questioned whether the "trend" seen in the diagrams implies a genetic relationship, a least squares approximation technique has been introduced in order to determine whether the composition of the main components of a rock (F) can be expressed by the linear combination of a selected set of compositions of a magma and the phenocrysts crystallized from it : F(o)=F(1)x(1)+F(2)x(2)+······+F(m)x(m) ······(1) where F(1), F(2), ... denote the compositions of a magma and minerals, and F(o) is the calculated composition of F. These calculations lead to the conclusion that there are at least two series of rocks in Asama (Tables 25 to 30 and Fig. 9), distinguished from each other mainly by their K(2)O content. Those rocks showing features of assimilation (Aramaki, 1963) all belong to the K(2)O-rich series. Contents of minor components such as TiO(2), MnO, P(2)O(5) and SrO are analyzed by the linear regression technique in two ways, for example : TiO(2)(o)=C(1)x(1)+C(2)x(2)+ ······(2) and TiO(2)(o)=aMgO+bFe(o) +cK(2)O ······(3) These methods are found useful in discriminating rocks of different ongm and in distinguishing the characteristic behavior of each component. Results of calculations (Tables 31 to 34) support the conclusion reached by calculations based on the contents of major components.
Publication Title 岡山大学温泉研究所報告
Published Date 1963-10-25
Volume volume32
Start Page 1
End Page 85
ISSN 0369-7142
language Japanese
File Version publisher
NAID 120002310984