Conditions

close

result 48318 件

Author Mizukawa, Nobuyoshi| Tominaga, Susumu| Kimata, Yoshihiro| Onoda, Tomoo| Sugiyama, Narushi| Yamachika, Eiki| Yamada, Yousuke| Kimura, Takuji| Takeuchi, Tetsuo| Ueno, Takaaki| Takagi, Shin|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Minami, Hitoshi|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Yoshioka, Akihiko|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Yamamoto, Kazuhide|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Ueno, Katsumi|
Published Date 1993-02-27
Publication Title 岡山医学会雑誌
Volume volume105
Issue issue1-2
Content Type Journal Article
Author Seno, Shingo|
Published Date 1993-02-27
Publication Title 岡山医学会雑誌
Volume volume105
Issue issue1-2
Content Type Journal Article
Author Kitamura, Tomoki|
Published Date 1993-10
Publication Title 岡山医学会雑誌
Volume volume105
Issue issue9-10
Content Type Journal Article
Author Liu, Keyue| Mori, Shuji| Takahashi, Hideo| Tomono, Yasuko| Wake, Hidenori| Kanke, Toru| Sato, Yasuharu| Hiraga, Norihito| Adachi, Naoto| Yoshino, Tadashi| Nishibori, Masahiro|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Suehisa, Hiroshi| Toyooka, Shinichi| Hotta, Katsuyuki| Uchida, Akiko| Soh, Junichi| Fujiwara, Yoshiro| Matsuo, Keitaro| Ouchida, Mamoru| Takata, Minoru| Kiura, Katsuyuki| Date, Hiroshi|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
Author Toyota, Yuji|
Published Date 1993-02-27
Publication Title 岡山医学会雑誌
Volume volume105
Issue issue1-2
Content Type Journal Article
JaLCDOI 10.18926/ESR/13959
Title Alternative LISTHKL : List h, k, l, Fo and σFo tables
FullText URL ESR_1_49.pdf
Author Yamakawa, Junji| Kawahara, Akira|
Abstract LISTHKL, a Fortran 77 program listing up the data for deposit is submission to Acta Crystallo-graphica has been written. The program requires a computer set with a printer utilizung the LIPS3 page description language.
Keywords LISTHKL Acta Crystallographica reflection data
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 49
End Page 52
ISSN 1340-7414
language Japanese
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310510
JaLCDOI 10.18926/ESR/13958
Title Alternative CALCOMP to LIPS3 convert library
FullText URL ESR_1_37.pdf
Author Yamakawa, Junji|
Abstract CALLIP, a CALCOMP compatible Fortran 77 library using the Canon LIPS3 page description lan-guage, has been written. As a result, the graphic output of programs with CALCOMP plotting routines used for crystal structure analyses, such as ORTEP2, Rietveld analyses and others can be used under the printer equipped with LIPS3 PDL. The details of the library was given with some graphic examples.
Keywords CALLIP CALCOMP LIPS3 Fortran 77
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 37
End Page 48
ISSN 1340-7414
language Japanese
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310211
JaLCDOI 10.18926/ESR/13957
FullText URL ESR_1_27.pdf
Author Okano, Osamu| Nishiya, Nanayo| Kagami, Hiroo|
Abstract Rb-Sr isotopic study as well as petrologic investigations have been done on sixteen individul chondrule samples separated from the Allegan (H5) chondrite. The Rb-Sr chondrule isochron does not define a very precise age (4.42±0.17 Ga) and 87Sr/86Sr initial ratio (0.6997±0.0014) due to the very small variation in Rb/Sr ratio for the chondrules, whereas the model ages give a much more speciffic value (4.42±0.02 Ga). These ages may probably be indicative of the time of primary process (es) (e.g. chondrule formation) rather than secondary (metamorphic reheating) or tertiary (shock heating) processes in and/or on the H-chodrite parent body (or bodies). Chemical compositions of oliveines (Fa=17.5mol%, mean deviation (MD)=1.3%) and orthopyoxenes (Fs=15.4mol%, MD=3.2%) are moderately homogenized among the chondrules, while certains chemically uneguilibrated features are also distinctly preserved in this chondrite. Homogeneity of the mineral compositions, therefore, could not have been caused by thermal metamorphism but were probably inherited from processes prior to aggregation of the components. The overall implications of the chondrule isochron and model ages in relation to the petrological features and in comparison with Rb-Sr data of other chondrites of different chemical groups and petrologic types are discussed.
Keywords chondrule age Rb-Sr isochron Allegan H- chondrite meteorite metamorphism olivine pyroxene
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 27
End Page 36
ISSN 1340-7414
language English
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310261
Author Toyota, Yuji|
Published Date 1993-02-27
Publication Title 岡山医学会雑誌
Volume volume105
Issue issue1-2
Content Type Journal Article
JaLCDOI 10.18926/ESR/13955
Title Alternative ScSp Phase observed on the Coast of the Seto Inland Sea
FullText URL ESR_1_19.pdf
Author Nishi, Masaki| Oda, Hitoshi|
Abstract Observation of ScSp phase, P wave converted from ScS phase, has been made at a seismological observatory (SBK) located on the coast of the Seto Inland Sea, southwest Japan. The ScSp phases were found on the seismograms of earthqukes with long epicentral distances, but not observed for those with short epicentral distances. Such dependence of appearance of the ScSp phase on epientral distance is interpreted as being due to the Philippine Sea plate horizontally lying beneath the Shikoku and Chugoku districts.
Keywords ScS Phase ScSp Phase Philippine Sea Plate Southwest Japan
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 19
End Page 26
ISSN 1340-7414
language Japanese
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310571
Author Endo, Yoshikatsu| Sakai, Ryo| Ouchi, Masaaki| Onimatsu, Hideki| Hioki, Masayoshi| Kagawa, Shunsuke| Uno, Futoshi| Watanabe, Yuichi| Urata, Yasuo| Tanaka, Noriaki| Fujiwara, Toshiyoshi|
Published Date 2008-12-01
Publication Title 岡山医学会雑誌
Volume volume120
Issue issue3
Content Type Journal Article
JaLCDOI 10.18926/ESR/13953
FullText URL ESR_1_9.pdf
Author Suzuki, shigeyuki|
Abstract The Iberian Pyrite Belt is an Upper Paleozoic succession which has been divided into the Phyllite-Quartzite Group, the Volcanic-Sliceous Complex and the Culm Group in ascending order from base to the top. The contacts among them are conformable. These Groups are tightly folded and metamorphosed un-der low-grade conditions during Hercynian times. The first stage folds of the Volcanic-Siliceous Complex and the Culm Group are associate with slaty cleavages (S1), while the Phyllite-Quartzite Group is asso-ciate with schistosities (S1). Fold analysis using cleavages and minoe folds has been utilized in the analysis of the stratigraphy. This led to systematic horizontal collection of specimens (pelitic rocks). S1 texture is defined by paralled alignment of secondary platy minerals which tend to grow larger and together, forming zonal domains toward the Phyllite-Quartzite Group. The clay matrices change to recrystallized quartz toward the Phyllite Quartzite Group. Textural modifications are evidenced by gradational changes from slaty cleavages to schistosities. This shows that recrystallization is the important deformation mecha-nism responsible for S1 development. It also reflects that the deformation was contemporaneous with metamorphism.
Keywords Slaty cleavage Schistosity Recrystallization
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 9
End Page 18
ISSN 1340-7414
language English
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310428
JaLCDOI 10.18926/ESR/13952
FullText URL ESR_1_1.pdf
Author Nozaka, Toshio| Shibata, Tsugio|
Abstract Ultramafic rocks exposed around Mt. Ohsa(= Ohsa-yama), Okayama prefecture, designated as "Ohsa-yama ultramafic body" all together, are one of the Alpine-type peridotites in the Sangun metamorphic belt. They are intensely serpentinized and locally suffered contact metamorphism by younger granitic intrusions. In a por-tion of the ohsa-yama body where it has been affected by the contact metamorphism, the constituent minerals, texture and structure of primary ultramafic rocks have been locally preserved. Petrographic studies revead that the primary ultramafic rocks of the ohsa-yama body consist domimantly of dunite and harzburgite possessing no obvious layering, and their constituent minerals are similar in composition to those of the Tari-Misaka and Ashidachi ultramafic bodies. These features indicate that unlike the Ochiai-Hokubo body, the Ohsa-yama ultra-mafic body belongs to the "massive group" of the Arai's (1980) classification.
Keywords petrography dunite harzburgite massive ultramafic body
Publication Title Okayama University Earth Science Report
Published Date 1994-09-20
Volume volume1
Issue issue1
Start Page 1
End Page 8
ISSN 1340-7414
language English
Copyright Holders 岡山大学地球科学研究報告編集委員会
File Version publisher
NAID 120002310594