検索条件

閉じる

検索結果 18200 件

JaLCDOI 10.18926/ESR/13897
タイトル(別表記) Water-soluble materials formed by the reaction between a volcanic rock and HCI and/or SO2 gases
フルテキストURL ESR_7_21.pdf
著者 赤木 誠司| 山本 雅弘|
抄録 Experiments on the reaction of a volcanic rock, dacite with HCI and /or SO2 gases have been carried out at room temperature to 800℃ for understanding of the condition of the formation of water-soluble materials on volcanic ash. HCI reacted with the dacite mainly at low temperatures (≤200℃), whereas SO2 did at high temperatures (≥400℃). It was also found that CI/SO4 ratios of water-soluble materials were very high at low temperatures, but decreased rapidly with increasing temperature. In the experiments using a mixture of HCI and SO2, the cation composition at 600℃ and 800℃ was revealed to be significantly different from that at lower temperatures, suggesting the change in the reaction process with temperature.
キーワード Volcanic gas Volcanic ash Water-soluble material CI/SO4 ratio
出版物タイトル Okayama University Earth Science Report
発行日 2000-09-20
7巻
1号
開始ページ 21
終了ページ 26
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310554
著者 城市 康隆| Narong, Lenghor| 高柳 俊夫| 大島 光子| 本水 昌二| 浦 信夫|
発行日 2006-11-17
出版物タイトル 分析化学
55巻
9号
資料タイプ 学術雑誌論文
著者 山縣 浩一|
発行日 1993-08
出版物タイトル 岡山医学会雑誌
105巻
7-8号
資料タイプ 学術雑誌論文
JaLCDOI 10.18926/ESR/13894
タイトル(別表記) Native gold from Mikawa mine, Niigata Prefecture, Japan
フルテキストURL ESR_7_19.pdf
著者 山川 純次| 田邊 満雄| 島田 和昌| 逸見 千代子|
抄録 Native gold was found at Mikawa mine, Niigata Prefecture, Japan. The mineral was associated with quartz in a druse within quartz-vein in propyrite. The crystals were formed in filiform, reticulated and dendritic shapes with about 1 mm length with 0.1 mm width and 0.05 mm thickness. Very malleable and ductile, opaque and yellow with metallic luster. Qualitative and semi-quantiative analyses were performed by the wavelength dispersive EPMA. Quantitatively, the crystals contained Au, Ag and Hg. Semi-quantitative analyses were executed with ZAF correction algorithm. The results showed that these specimens had a average chemical composition Au0.77 Ag0.11Hg0.12. This specimen was archived at our site with a collection number ESO-M01001.
キーワード Native Gold Mikawa Mine electrum ESO-M01001
出版物タイトル Okayama University Earth Science Report
発行日 2000-09-20
7巻
1号
開始ページ 19
終了ページ 20
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310280
JaLCDOI 10.18926/ESR/13893
フルテキストURL ESR_7_15.pdf
著者 小田 仁| Ito Aki|
抄録 Long-period coda waves were recorded on the vertical-component seismograms of aftershocks of the Hyogo-ken Nanbu earthquake, 1995. We identify the long-period coda waves as Rayleigh wave, because they appear after the S-arrival times and exhibit the normal dispersion that propagation velocity of the coda waves increases with an increase in period. By applying the moving window analysis to the coda waves from nine aftershocks, the group velocities are determined as a function of period within the range of 2 to 8 s. The group velocity dispersion data are inverted to investigate the S-wave velocity structure of the upper crust. The S-wave velocity structure is consistent with those obtained in previous studies using traval time analysis of bood waves.
キーワード surface wave dispersion coda wave S-wave velocity structure upper crust Hyogo-ken
出版物タイトル Okayama University Earth Science Report
発行日 2000-09-20
7巻
1号
開始ページ 15
終了ページ 18
ISSN 1340-7414
言語 英語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310493
JaLCDOI 10.18926/ESR/13891
タイトル(別表記) Automated observation of sea surface eddy flux on a cruising ship
フルテキストURL ESR_7_1.pdf
著者 高橋 聡司| 塚本 修| 石田 廣史| 米山 邦夫|
抄録 Sea surface eddy fluxes were evaluated with the eddy correlation method including ship motion correction for the wind vector components. Previous ship motion correction algorithm was revised as a simple scheme setting a motion sensor at the same place with the sonic anemometer. This revised eddy flux system was mounted as a routine continuous measurement system on the R/V 'Mirai' of Japan Marine Science and Technology Center. The first cruise was conducted at the tropical weatern Pacific in June 2000. Continuous sea surface fluxes were obtained and the data quality was checked with some parameters. This system is planned to be developed as a automated data processing system including ship motion correction and real-time flux evaluation system. These eddy fluxes can be integrated with the bulk fluxes and radiation fluxes to understand sea surface heat balance over the global ocean.
キーワード Sea surface fliux Automated observation Eddy correlation method
出版物タイトル Okayama University Earth Science Report
発行日 2000-09-20
7巻
1号
開始ページ 1
終了ページ 14
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310644
著者 山本 貴子| Akhmad, Sabarudin| 野口 修| 高柳 俊夫| 大島 光子| 本水 昌二|
発行日 2006-11-17
出版物タイトル 分析化学
55巻
9号
資料タイプ 学術雑誌論文
JaLCDOI 10.18926/ESR/13888
タイトル(別表記) Relationship between the water quality of three main rivers and geology of Okayama Prafecture
フルテキストURL ESR_8_1_29.pdf
著者 木下 卓也| 松田 敏彦|
抄録 Concentrations of inorganic major components (Ca2+, Mg2+, Na+, K+, ΣFe, AI3+, HCO3, SO4, CI-, NO3, F- and SiO2) were measured in 57 water samples from three main rivers, the Yoshii, Asahi and Takahashi Rivers and their tributaries. The water quality is discussed in relation to the geological environment in the drainage basin of three rivers. The following results were obtained from the investigation. The degree of influence of rocks on the water quality was limestone≫basic rocks>clastic rocks>andesite>rhyolite>gramite. The influence of geology is clear in the riverhead but it is obscure in the downstream. The concentration of each component increases generally from the upper stream to the lower stream but that of SiO2 only decreases in the lower stream. Kaolinite is a stable mineral as a weathering prodouct from the ion compositions of three rivers. In a rough estimation, Yoshii, Asahi and Takahashi Rivers weather 303,000t, 433,000t and 1,033,000t of the rocks respectively from their basins in a year. The syrface of their basins are scraoed off 0.06mm, 0.11mm and 0.15mm respectively in a year.
キーワード Water quality River water Geology of basin Yoshii River Asahi River Takahashi River Okayama Prefecture
出版物タイトル Okayama University Earth Science Report
発行日 2001-09-20
8巻
1号
開始ページ 29
終了ページ 38
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310339
JaLCDOI 10.18926/ESR/13887
タイトル(別表記) Trace of the Median Tectonic Line in Mima area, eastern Shikoku
フルテキストURL ESR_8_1_13.pdf
著者 水井 良暢| 橘 徹| 鈴木 茂之|
抄録 Tracing outcrops of shear zone were used to describe the geometry and structure of the Median Tectonic Line in Mima area, eastrn Shikoku. A distinct new fault outcrop was discovered between the Mino and Ikuchi Faults at the northern slope of the Mt. Boso. These two faults are regarded as a single continuous fault. The analysis of surface fabrics of quartz in fault in fault gauge has been carried out to determine relative fault activity events.
キーワード surface fabrics fault gauge Mino-Ikuchi Fault Median Tectonic Line
出版物タイトル Okayama University Earth Science Report
発行日 2001-09-20
8巻
1号
開始ページ 13
終了ページ 28
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310656
著者 木村 康裕|
発行日 1994-12
出版物タイトル 岡山医学会雑誌
106巻
11-12号
資料タイプ 学術雑誌論文
JaLCDOI 10.18926/ESR/13885
タイトル(別表記) Miocene Ukan Formation, Ukan Area, Okayama Prefecture, Southwest Japan
フルテキストURL ESR_8_1_1.pdf
著者 藤原 貴生| 田口 栄次| 鈴木 茂之|
抄録 In this paper, we deal with the Miocene Ukan Formation, sporadically distributed in Ukan-cho, Okayama prefecture, from a viewpoint of analysis of lithology and molluscan assemblages. The Ukan Formation is lithostratigraphically divided into the Suzuoka Conglomerate, Yamagata Muddy Sandstone, Shimoyokomi Sandstone and Conglomerate, Azechi Sandstone and Conglomerate, Tsuneyama Siltstone Members in ascending order. The following 6 molluscan assemblages are recognized. The lower four members and the last member is correlative to the Lower Sandstone and Upper Shale Formation of the Bihoku Group, respectively judging from lithology and fauna. The temporal chages of the above mentioned molluscan assemblages represents that gradual deeping of sea during the depositional period from the Suzuoka Conglomerate and Yamagata Muddy Sandstone Members to the Azechi Sandstone and Conglomerate Member via the Shimoyokomi Sandstone and Conglomerate Member, and abrupt deeping of sea seems to have happened between the Azechi Sandstone and Conglomerate Member and the Tsuneyame Siltstone Member.
キーワード Lithology Molluscan assemblage Paleoenvironmental change Ukan Miocene
出版物タイトル Okayama University Earth Science Report
発行日 2001-09-20
8巻
1号
開始ページ 1
終了ページ 12
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310604
著者 宮下 雄博|
発行日 1993-08
出版物タイトル 岡山医学会雑誌
105巻
7-8号
資料タイプ 学術雑誌論文
著者 藤原 貴生| 鈴木 茂之|
発行日 2002-09-20
出版物タイトル Okayama University Earth Science Report
9巻
1号
資料タイプ 紀要論文
著者 Saieev K| 小山内 康人|
発行日 2002-09-20
出版物タイトル Okayama University Earth Science Report
9巻
1号
資料タイプ 紀要論文
著者 入江 正一郎|
発行日 1994-12
出版物タイトル 岡山医学会雑誌
106巻
11-12号
資料タイプ 学術雑誌論文
JaLCDOI 10.18926/ESR/13876
タイトル(別表記) A note on dental nomenclature in the Rhinocerotidae
フルテキストURL earth_science_reports_010_1_33.pdf
著者 福地 亮|
抄録 The terminology for the molars of rhinoceorses is mainly derived from Osborn (1888). However, there is often confusion surrounding nomenclature of cheek teeth and the measuring point of the teeth. The nomenclature for the teeth of rhinoceroses and the controversy were reviewed. In this paper, I suggest the new nomenclatures that are composed of 24 elements for the upper cheek teeth and 12 ones for the lower ones and I also suggest the measuring points of teeth of the Rhinocerotidae.
キーワード teminology teeth rhinoceros
出版物タイトル Okayama University Earth Science Report
発行日 2003-12-20
10巻
1号
開始ページ 33
終了ページ 37
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310241
JaLCDOI 10.18926/ESR/13875
タイトル(別表記) Depositional environments of the Katsuta Group, eastern Tsuyama Basin, Southwest Japan
フルテキストURL earth_science_reports_010_1_23.pdf
著者 山崎 良| 鈴木 茂之|
抄録 The Miocene Katauta Group of the Syohoku-cho area is subdivides into 6 members ; The Uetsuki Conglomerate Member, Nara Sandy Mudstone Member, Tai Gravelly Sandstone Member, Takatori Conglomerate Member, Ayabe Mudstone Member and Maruyama Mutstone Member from bottom to top. The unconformity between Miocene deposits and basement rocks in this area was traced to obtain geometry of the Miocene basin. Contour maps of the bases of the Miocene Yoshino Formation and Takakura Formation indicate paleo-topography. The obtained topography demonstrates a valley, which flowed to north-west, and a few islands and bays. It indicates that these Miocene successuions were deposited in the topography which resemble to the present Seto Inland.
キーワード Katsuta Group Tsuyama Basin Miocene geometry of basin paleoenvironmental chage
出版物タイトル Okayama University Earth Science Report
発行日 2003-12-20
10巻
1号
開始ページ 23
終了ページ 31
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310475
JaLCDOI 10.18926/ESR/13874
タイトル(別表記) Distributions and ages of the Paleogene deposits in the Kibi Plateau Area, and Paleogene paleogeography
フルテキストURL earth_science_reports_010_1_15.pdf
著者 田中 元| 鈴木 茂之| 宝谷 周| 山本 裕雄| 壇原 徹|
抄録 The "Kibi Plateau" forms a unique geomorphic province with the gently-sloping and stable continental feature. Gravel deposites called the "Mountain Gravels", are distributed sporadically in the Kibi Plateau, and have been considered Pliocene deposits. However, recent fission-track ages of the tuff beds intercalated in the deposits have indicated that the ago of deposits are Paleogen in the age. So far, fission-track ages (using zircon) of 61 to 65, 55, 37, 34 to 35 and 27 Ma are obtained. Remaining the belt-like distributions of the Paleogene gravelly valley-full deposits suggest that the Kibe Plateau has been keeping as a stable block, and repeated periods of incision followed by sedimentation of valley-fill deposits are occurred in the area during Paleogene period.
キーワード Kibi Plateau gravelly valley-fill deposites fission-track ages Paleogene palaeogeography
出版物タイトル Okayama University Earth Science Report
発行日 2003-12-20
10巻
1号
開始ページ 15
終了ページ 22
ISSN 1340-7414
言語 日本語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310517
JaLCDOI 10.18926/ESR/13873
フルテキストURL earth_science_reports_010_1_11.pdf
著者 鈴木 功| 井上 靖| 小田 仁| 森岡 正名|
抄録 Resonant frequencies for a single crystad diopside sphere are measured accurately and rhirteen elastic moduli are reluced by the least squares calculation, A set of mduli gives theoretical resonant frequencies close enough to the observed ones.
キーワード diopside single crystal resonace sphere elasticity
出版物タイトル Okayama University Earth Science Report
発行日 2003-12-20
10巻
1号
開始ページ 11
終了ページ 14
ISSN 1340-7414
言語 英語
著作権者 岡山大学地球科学研究報告編集委員会
論文のバージョン publisher
NAID 120002310552
著者 宮下 雄博|
発行日 1993-08
出版物タイトル 岡山医学会雑誌
105巻
7-8号
資料タイプ 学術雑誌論文