| JaLCDOI | 10.18926/ESR/13857 |
|---|---|
| タイトル（別表記） | Drilling Research of a high-latiude coral reef in Mage Island, Stsunan Islands, Japan |
| フルテキストURL | ESR_12_49.pdf |
| 著者 | 菅 浩伸| 中島 洋典| 大橋 倫也| 濱中 望| 岡本 健裕| 中井 達郎| 堀 信行| |
| 抄録 | Four drilling cores are observed from a high-latitude coral reef at the northwestern Mage Island (N30゜45' 40"). The thickness of the Holocene reef is around 2.5m in the reef edge and 4m in back reef. The Holocene thickness is relatively thin comparing to the modern reefs in the middle or the southern Ryukyu Islands. The reef structure Acropora facies, reworked coral rubble facies. This zonal structure conforms to the ecological coral-zonation corresponding to the wave-energy gradient. |
| キーワード | Holocene Coral Reef Sedimentary Structure Drilling Southwestem Japan |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 49 |
| 終了ページ | 58 |
| 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 | 120002310535 |
| JaLCDOI | 10.18926/ESR/13856 |
|---|---|
| タイトル（別表記） | Local wind storm (Hirodo-kaze) in northern Okayama caused by Typhoon 0421 & 0423 |
| フルテキストURL | ESR_12_39.pdf |
| 著者 | 片岡 文恵| 塚本 修| |
| 抄録 | In 2004, ten typhoons had landed over Japan and a lot of damages were reported due to heavy rain, storm surge and wind storms. In the north eastern part of Okayama prefecture, local high wind "Hirodo-kaze" caused severe wind damages due to typhoon passage. During Typhoon 0421, high winds were recoreded in the south foot of Mt.Nagi as typical local wind atrom, " Hirodo-kaze". While, during Typhoon 0423, severe wind damages expanded west of the typical Hirodo-kaze srea as well as a new extreme. In the present report, a lot of surface meteorological data were coollected and compared the meteorological fields among two typhoons. |
| キーワード | Wind Storm Hirodo-kaze Typhoon Local high wind |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 39 |
| 終了ページ | 47 |
| 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 | 120002310608 |
| JaLCDOI | 10.18926/ESR/13855 |
|---|---|
| タイトル（別表記） | 中国淮河流域付近の入梅前の時期における大気場や陸面状態の季節進行 (1998年の事例解析) |
| フルテキストURL | ESR_12_31.pdf |
| 著者 | 池田 祥一郎| 加藤 内藏進| 塚本 修| |
| 抄録 | Seasonal evolution of atmospheric and land surface conditions around the Huaihe River Basin in China in the pre-Meiyu stage of 1998 were examined, mainly based on the GAME re-analysis data. Around the Huaihe River Basin in China (just to the nront of the Changjiang River Basin), although the air temperature increased rapidly already in early June (the Meuyu front was located to the south of that region), the specific humidity did not increas so much at time. In addition, the latent heat supplied from the ground there decreased from late May to early June, compared to that before early May. The time mean southerly wind component across the low-level baroclinic Zone (although not so strong as in the mature stage of the Meiyu) invaded into Central Cjina during late April to early May. On the other hand, the relatively strong wind region once retreated southward in the middle of May associated with the onset of the Southeast Asian monsoon, and the calm wind region with frequent appearance of the surface high was seen around the Huaihe River Basin from late May to early June. Thus the present study shows that the Huaihe River Basin once experiences the rather drier stage just before the onset stage of the mature Meiyu there. |
| キーワード | arid region in China and the Meiyu front seasonal evlution in East Asia Land surface condition around the Meiyu front |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 31 |
| 終了ページ | 37 |
| 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 | 120002310602 |
| JaLCDOI | 10.18926/ESR/13853 |
|---|---|
| タイトル（別表記） | ガーナ,南部アシャンティ帯の原生代プリンスタウン・グラニトイド岩体に関する主成分地球化学 |
| フルテキストURL | ESR_12_15.pdf |
| 著者 | Samuel Dampare| 柴田 次夫| Daniel Asiedu| Shiloh Osae| |
| 抄録 | The Pateoproterozoic metavolcanic rocks of the southern Ashanti greenstone belt of Ghana are intruded by three major suites of granitoids, locally called Prince's Town, Dixcove and Ketan plutons. The Prince's Town pluton is the largest intrusive body in the Axim area, and tends to separate the Axim volcanic branch from the Cape Three Points branch. The Pluton consists of granitic to dioritic rocks, which are generally massive but occasionally display alignment of ferromagnesian minerals. The rocks contain mainly plagioclase, K-feldspar, quartz, amphibole, biotite and opaques. The feldspars are mostly sericitized and saussuritized, and alteration of amphibole and biotite to epidote and chlorite is common. Accessory minerals include apatite, sphene and zircon. The geochemical data indicate that the rocks are tonalitic to granodioritic in composoition, metaluminous (ASI<1) and have I-type characteristics. The granitoids have the SiO2 content of 63-70% ; total iron, as Fe2 O3 of 3.10-5.80% ; (Na2O+K2O) content of 5.01-6.96% and Na2O/K2O ratios from 1.34 to 2.70 ; and are characterized by Mg# ranging from 53 to 48. The Fe*(=FeOtot/FeOtot+MgO) and modified alkali-lime index (MALI) of the rocks indicate that the Prince's Town pluton is dominantly magnesian and calcic in nature. Higher values in molar CaO/(MgO+FeOtot) coupled with low molar AI2O3/(MgO+FeOtot) may suggest their derivation from partial melting of metabasaltic to metatonalitic sourcc, with a possible contribution from metagreywacke, but preclude any contribution from metapelitic sources. The Birimaian metavolcanic rocks are the likely source material candidate for the rocks. CIPW norm calculations yielded a crystallization temperature of～650-685℃ and a pressure of 4-7kb for the rocks, suggesting a lower crustal souree. The Prince's Town plutonic rocks also show characteristice of plutons emplaced in a volcanic are tectonic setting environment. This observation is largely consistent with previous studies conducted on granitoids from other parts of the southern Ashanti greenstone belt c and the belt-type granitoids of Ghana as a whole. |
| キーワード | Geochemistry tectonic setting granitoids Birimian Ghana |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 15 |
| 終了ページ | 30 |
| 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 | 120002310649 |
| JaLCDOI | 10.18926/ESR/13851 |
|---|---|
| タイトル（別表記） | ガーナ, ビルム・ダイヤモンド産地のアクァティア地域に分布する沖積層の重鉱物分析 |
| フルテキストURL | ESR_12_7.pdf |
| 著者 | Samuel Dampare| Daniel Asiedu| Bruce Banoeng-yakubo| 柴田 次夫| |
| 抄録 | Heavy mineral analysis was carried out on Pliocene to Recent alluvial sediments from the Birim diamondiferous field od Ghana. The main objective of the study was to examine the mineral composition of heavy fractions in order to identify : (1) the heavy mineral assenblage that occur in the sediments, (2) particular diamond indicator minerals associated with the diamonds, and (3) the provenance of the alluvial sediments. The heavy minerals are essentially composed of staurolite, ilmenite and magnetite in varying proportions, with trace amounts of leucoxene, rutile, garnet and zircon. The heavy mineral assenblage and chemical composition of ilmenite and gamet suggest their derivation from phyllites and schists which reflect directly the composition of the basement rocks developed in the study area. The absence of diamond indicatior minerals such as apatite, pyrope garmet, chromian spinel, and picroilmenite in the heavy fraction is unlikely to be due to their destruction during intense weathering and/or diagenesis but rarher their non-occurrence in the area. |
| キーワード | Heavy minerals provenance sediments diamonds Ghana |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 7 |
| 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 | 120002310657 |
| JaLCDOI | 10.18926/ESR/13850 |
|---|---|
| タイトル（別表記） | 沖縄トラフ第四与那国海丘海底熱水系チムニーの錫を含む黄銅鉱と白金を含む輝蒼鉛鉱 |
| フルテキストURL | ESR_12_1.pdf |
| 著者 | Gena, Kaul| 千葉 仁| 加瀬 克雄| |
| 抄録 | The active sulfide chimney ore sampled from the flank of the active Tiger chimney in the Yonaguni Knoll IV hydrothermal system, South Okinawa Trough, consists of anhydrite, pyrite, shalerite, galena, chalcopyrite and bismuthinite. Electron microprobe analyses indicated that the chalcopyrite and bismuthinite contain up to 2.4 wt. % Sn and 1.7 wt. % Pt, respectively. The high Sn-bearing chalcopyrite and Pt-bearing bismuthinite are the first occurrence of such minerals on the submarine hydrothermal systems so far reported. The results confirm that the Sn enters the chalcopyrite as a solid solution towards stannite by the coupled substitution of Sn 4+ Fe 2+ for Fe 3+ Fe 3+ while Pt enters the bismuthinite structure as a solid solution during rapid growth. The homogenization temperature of the fluid inclusions in anhydrite (220-310℃) and metasured end-member temperature of the vent fluids (325℃) indicate that the minerals are precipitated as metastable phases at temperature around 300℃. The Sn-bearing chalcopyrite and Pt-bearing bismuthinite expess the original composition of the minerals deposited from a hydrothermal fluid with temperatures of about 300℃. |
| キーワード | Sn-bearing chalcopyrite Pt-bearing bismuthinite Active sulfide Chimmey Yonaguni Knoll IV Okinawa Trough seafloor hydrothermal system |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2005-12-31 |
| 巻 | 12巻 |
| 号 | 1号 |
| 開始ページ | 1 |
| 終了ページ | 5 |
| 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 | 120002310444 |
| JaLCDOI | 10.18926/ESR/13848 |
|---|---|
| タイトル（別表記） | Eastward extension of the Baiu Front on the surface weather maps in ralation to zonal scale of the area with strong low-level southerly wind toward the front |
| フルテキストURL | EAR_13_1_19.pdf |
| 著者 | 中山 祐貴| 大和田 道雄| 池田 祥一郎| 加藤 内藏進| |
| 抄録 | Eastward extension of the Baiu front in relation to zonal scale of the area with strong low-level southerly wind toward the front was examined based on the operational surface weather maps and the NCEP/NCAR re-analysis data mainly for the mature Baiu period (15 June to 31 July) from 1991 to 2000. During that period, the Baiu front on the surface weather maps appeared from the Changjiang River Basim to the east of the Japan Islands accompanied by the strong low-level southerly wind toward it in a wide zonal scala(～3500km), in many cases. However, the situations when the appesrance of the Baiu front was limited to the western part of the Japan Islands or limited to its eastern part are sometimes found with relatively narrow zonal acale of the strong low-level southerly wind toward the front, although the appearance frequency of such cases was not so high. As such the present results illustrate the importance of the zonal scale of the subtropical high for the spatial activity of the Baiu front. |
| キーワード | variation of the Baiu front southerly wind in the subtropical high area zonal extension of the Baiu front |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2006-03-31 |
| 巻 | 13巻 |
| 号 | 1号 |
| 開始ページ | 19 |
| 終了ページ | 25 |
| 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 | 120006211873 |
| JaLCDOI | 10.18926/ESR/13847 |
|---|---|
| タイトル（別表記） | Geology of Holocene deposits in Mizushima Area, Okayama Prefecture, Japan |
| フルテキストURL | EAR_13_1_15.pdf |
| 著者 | 鈴木 茂之| |
| 抄録 | The study srea, Mizushima is occupied by polder and reclaimed land. The ground of this area is composed of the Holocene deposits below the surface. The deposits are mostly 10 to 20m in thickness and composed of 2 units, the B Unit and C&D Unit. The B Unit is composed of muddy sand with 2 to 3m in thickness. This unit is thought to be deposited in the mouth of paleoriver. The C&D Unit is composed of marine mud and sand with 10 to 15m in thickness. This unit is especially soft and will expand ground oscillations during an earthquake. |
| キーワード | Holocene deposits Mizushima Area Ground oscillation |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2006-03-31 |
| 巻 | 13巻 |
| 号 | 1号 |
| 開始ページ | 15 |
| 終了ページ | 18 |
| 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 | 120002310562 |
| JaLCDOI | 10.18926/ESR/13844 |
|---|---|
| タイトル（別表記） | バングラディシュの更新世台地の地形と地質 |
| フルテキストURL | EAR_13_1_1.pdf |
| 著者 | Towhida Rashid| Md. hossain Monsur| 鈴木 茂之| |
| 抄録 | With regards to the origin and evolution of the Pleistocene tracts (Lalmai, Madhupur and Barind tracts) of Bangladesh, two trends of thoughts are common. Most of the authors believed that the Madhupur, Barind and Lalmai tracts represent tectonically uplifted surface. Some researchers have different opinion and they believed that the Lalmai hills and the Madhupur locality represent tectonically uplifted blocks but the whole Barind tract and the major portion of the Madhuput tracts are not tectonically uplifted, rather these are originated by erossional-depositional processes. In order to solve the problems associated with origin and evolution of Pleistocene tracts of Bangladesh, further study is needed. Borehole data may be collected and fusion images can be prepared from aerial photographs and setellite images to detect netectonic imprins and geomorphological signatures of the areas. Elaborate laboratory analysis of sediment deposits, radiocarbon dating my indicate a new dimension about the origin and evolution of these tracts. |
| キーワード | Bangladesh Lalmai Hill Barind Tract Madhupur Tract Neotectonices Aerial photographs Satellite Image Fusion Image |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2006-03-31 |
| 巻 | 13巻 |
| 号 | 1号 |
| 開始ページ | 1 |
| 終了ページ | 13 |
| 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 | 120002310445 |
| JaLCDOI | 10.18926/ESR/13828 |
|---|---|
| タイトル（別表記） | Storm surge in the Seto Inland Sea accompanied by Typhoons in 2004 |
| フルテキストURL | earth_science_reports_014_1_1.pdf |
| 著者 | 淺沼 友光| 塚本 修| 小川 貢司| |
| 抄録 | In 2004, Seto Inland Sea coast suffered severe damages of storm surge. This area never experienced storm surge damage in recent half century and people were not ready for the storm surge. In two typhoons of T0416 and T0418, surge anomaly were more than 150cm in Bisan-Seto area. Storm surges appeared after the maximum approach of typhoon not only due to surface low pressure but also due to wind stress as westerly. Because of geographical complexity of Seto Inland Sea, the surge process have not been well understood. Therefore, it is necessary to study the effects of the wind and the surface pressure using a numerical model. Atmospheric model MM5 and ocean model POM were used as a numerical experiment, including the astronomical tide model NAO. Aｓ the results of numerical simulation of the storm surge, atmospheric conditions were well simulated but ocean model was rather complex. There are a lot of island in Seto Inland Sea and sea water movement in the model was very much influenced by the topography and wind stress effect appeared much smaller. In the no-island model, storm surge height was a little improved. However the simulated surge height was still less than the observed height. Further improvement of the ocean model application should be considered in future studies. |
| キーワード | Typhoon Storm Surge Seto Inland Sea surface pressure wind stress |
| 出版物タイトル | Okayama University Earth Science Report |
| 発行日 | 2008-03-31 |
| 巻 | 14巻 |
| 号 | 1号 |
| 開始ページ | 1 |
| 終了ページ | 9 |
| 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 | 120002310572 |
| 著者 | 石田 聡子| |
|---|---|
| 発行日 | 2007 |
| 出版物タイトル | 北東アジア経済研究 |
| 巻 | 6巻 |
| 号 | 1号 |
| 資料タイプ | 紀要論文 |
| JaLCDOI | 10.18926/13320 |
| JaLCDOI | 10.18926/13317 |
|---|---|
| タイトル（別表記） | Regional Disparity Problem and Its Structure in the East Region of EU |
| フルテキストURL | 6_045_058.pdf |
| 著者 | 田口 雅弘| |
| 抄録 | 本稿は､EU東部地域の経済格差の現状をＥＵ中心部との比較､また国内における県別の比較を行い､その構造を明らかにするものである｡ 1997年 7月に欧州委員会は｢アジェンダ2000｣を発表した｡これによって､ポーランドを含む旧東欧 5カ国およびキプロスの先行加盟が準備され始める｡こうした動きに並行して､コソヴォ紛争の深刻化などに伴い､ＥＵは｢拡大によるＥＵの安定化｣志向を強めることとなる｡最終的には､2004年に10ヵ国､2007年に 2ヵ国が新規に加盟した｡ ＥＵ東方拡大は､全般的にはＥＵの政治的･経済的安定化に貢献したが､しかしながら､地域経済圏拡大はかならずしもクロスボーダーリージョンの安定化につながっているわけではない｡むしろ､ＥＵ拡大によって生じた摩擦や対立もある｡それは､現在ＥＵ内で急速に拡大志向の議論が萎み､｢拡大｣よりは｢深化｣に重点を置く議論が中心になりつつあることにも表れている｡もちろん､その背景には､｢拡大｣が経済圏･文明圏として重要な地域をほぼ包括しつつあること､ＥＵ周辺の政治的混乱が収まりつつあることなどがあるだろう｡しかしその一方で､拡大によって逆に多様性＝不安定要素を取り込んでしまい､その対応に多くの労力と資金がつぎ込まれて､拡大のメリットが十分に享受できないという｢拡大疲れ｣を伴った不満もある｡ 本稿では､経済格差､経済発達の遅れがどの程度のレベルにあるかを､ポーランドを中心に統計的に整理し､その構造を明らかにすることによって､クロスボーダーリージョン安定化を考える上でのひとつの材料としたい。 |
| 出版物タイトル | 北東アジア経済研究 |
| 発行日 | 2008 |
| 巻 | 6巻 |
| 号 | 1号 |
| 開始ページ | 45 |
| 終了ページ | 58 |
| ISSN | 1880-8476 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310248 120002310248 |
| JaLCDOI | 10.18926/13316 |
|---|---|
| フルテキストURL | 6_037_044.pdf |
| 著者 | 榎本 悟| |
| 抄録 | As everybody knows, China is growing very rapidly since the opening of the country in 1978.The real Gross Domestic Product (GDP) of China in 2006 has more than 13 times larger than that of 1978. If we suppose the real GDP in 1978 is 100, then we can get 1335 in 2006. Also, the real growth rate of China is almost 10％ annually during the same period ( Ke,2006) and people in the world are amazed to know it. It is often said that the sum of China's GDP will surpass Japan's within a decade or less, if China continues to grow. With the continuation of the growth of Chinese economy, many companies in the world, especially US, European and Japanese companies have already gone into China either to produce goods for exporting back to home country or to foreign countries (export market-oriented) or to produce goods for Chinese domestic market (domestic market-oriented) or both, in any case, exploiting the use of inexpensive labor forces. In fact, foreign countries, of course the main actors are multinational corporations (MNCs) , have heavily invested in China. For example, the total accumulated amount of foreign direct investment (FDI, stock base) from Japan to the world has amounted to $449.6bn. in 2006, of which China has received $30.3bn. (6.3％) , the fourth rank, following the U.S. ($156.4bn., 34.8％) , Holland ($45.4bn., 10.1％) , and U.K. ($31.6bn., 7.0％) . Even on the flow basis, China has received $63.0bn. of inward investment in 2006, of which the most important investing country to China is Hong Kong, totaling $20.2 bn. in 2006, followed by UK-held Virgin Island ($11.2 bnJ ,the second rank, Japan ($4.6bnJ ,the third rank, South Korea ($3.9bnJ and the U. S. ($2.7bn) . (China Statistical Yearbook 2007; JETRO White Paper: Trade and Investment 2007) Based on the above-mentioned facts, we consider the competitive situations among companies from different countries in China. Do they compete head-to-head? Or, do they compete in another way? Through the executives' perception on competition, we try to deal with how they feel their competitive situation in China, based on a questionnaire survey which was sent to Japanese executives in charge of managing manufacturing subsidiaries in China during September to October in 2004 to investigate how subsidiary executives feel their competitive situation there and what kind of strategy they should pursue in the coming years. This paper comprises 4 sections. The next section shows how we collected companies' data, operating in China, and what kind of criteria we have employed to do the research and the basic features of responding companies. The third section deals with the perception of executives on how they perceive their conditions of Chinese market in relation to the competition with their competitors. And we also introduce Porter's Five forces model to investigate why they feel about their market. The final section argues that we have to consider how Japanese executives respond to the competitive situation. Hence, a managerial implication will be discussed from the standpoint of Japanese executives. |
| 出版物タイトル | 北東アジア経済研究 |
| 発行日 | 2008 |
| 巻 | 6巻 |
| 号 | 1号 |
| 開始ページ | 37 |
| 終了ページ | 44 |
| ISSN | 1880-8476 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002310523 |
| JaLCDOI | 10.18926/13315 |
|---|---|
| フルテキストURL | 6_021_036.pdf |
| 著者 | Huang Shaoan| Gao Wei| Zhang Su| Huang Naijing| |
| 抄録 | This paper tries to measure the effect of cooperation on economic growth of both China and Japan by setting up an econometric model. This measuring is based on the basic framework of cooperation economics (Huang shao-an,2000) . The structure of the paper is as follows: The first part introduces the basic idea and analytical methods of cooperation economics; the second part establishes an econometric model for measuring the effect of cooperation on economic growth of both China and Japan; The third part measures degree of cooperation between China and Japan from two dimensions which are political factor and bilateral trade between China and Japan, and lists all the macroeconomic data that the econometric model needs; The fourth part employs the econometric model and the macroeconomic data to calculate the effect of cooperation on economic growth of both China and Japan; the final part is a brief conclusion. |
| 出版物タイトル | 北東アジア経済研究 |
| 発行日 | 2008 |
| 巻 | 6巻 |
| 号 | 1号 |
| 開始ページ | 21 |
| 終了ページ | 36 |
| ISSN | 1880-8476 |
| 言語 | 英語 |
| 論文のバージョン | publisher |
| NAID | 120002310579 |
| JaLCDOI | 10.18926/13314 |
|---|---|
| タイトル（別表記） | Current Progress Stage of the Chinese Economy and Its New Role in East Asian Economic Cooperation |
| フルテキストURL | 6_005_020.pdf |
| 著者 | 趙 偉| |
| 抄録 | 東アジア経済協力を論ずる際に､中･日･韓三国の役割を忘れてはならない｡特に中国という要素を忘れてはならない｡また東アジア経済協力における中国という要素を論ずるに当たって､一つの現実的問題-すなわち､最近20年以上にわたる中国経済の非常に急速な成長-を見逃してはならない｡この中国の急速な成長は､積極的な対外開放戦略に大きく依存して実現されているからだ｡東アジア経済協力における中国の地位と役割には､大きな変化が生じつつある｡この点には疑問の余地はない｡これは近年東アジア経済界で関心が高まっている問題の一つでもある｡しかし､これまで上記の問題を論じる際には､学界･実業界･政界のいずれにあっても､誰もが例外なく中国経済を (人口や国土面積などの)外面的要素から判断しようとしたことに留意しなければならない｡言い換えれば､中国以外の東アジア経済と比較した中国経済の規模から始まり､その影響力､ひいては東アジア経済協力における新たな地位について､外面的要素から判断しようとしたのは留意すべきことである｡一つの経済の外部に対する影響力は､その経済の外的な規模に限られるわけではなく､内部の社会経済発展と変化によっても決定される｡この点を認識できなければ､例えば､人口も国土面積も中国の最も小さな省より小さいスイスという国の世界と地域に与える影響力が､多くの中進国よりも大きい､という事実を理解できないだろう｡ このような認識に基づき､筆者は本論文で中国経済の内的発展段階の分析を出発点に､中国経済の東アジア経済協力における新たな地位と展望について論じたい｡ |
| 出版物タイトル | 北東アジア経済研究 |
| 発行日 | 2008 |
| 巻 | 6巻 |
| 号 | 1号 |
| 開始ページ | 5 |
| 終了ページ | 20 |
| ISSN | 1880-8476 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310317 |
| JaLCDOI | 10.18926/13313 |
|---|---|
| フルテキストURL | 6_001_002.pdf |
| 著者 | 清水 耕一| |
| 出版物タイトル | 北東アジア経済研究 |
| 発行日 | 2008 |
| 巻 | 6巻 |
| 号 | 1号 |
| 開始ページ | 1 |
| 終了ページ | 2 |
| ISSN | 1880-8476 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310441 |
| JaLCDOI | 10.18926/13307 |
|---|---|
| タイトル（別表記） | 在日留学生による第二・第三言語の使用における日本的文脈の役割 |
| フルテキストURL | 25_045_059.pdf |
| 著者 | 田中 共子| Simic Mira| |
| 出版物タイトル | 岡山大学大学院社会文化科学研究科紀要 |
| 発行日 | 2008-03-31 |
| 巻 | 25巻 |
| 号 | 1号 |
| 開始ページ | 45 |
| 終了ページ | 59 |
| ISSN | 18811671 |
| 言語 | 英語 |
| 著作権者 | 岡山大学大学院社会文化科学研究科 |
| 論文のバージョン | publisher |
| NAID | 120002310597 |
| 著者 | モハマド アルマヌル ラモン| |
|---|---|
| 発行日 | 2008-03-31 |
| 出版物タイトル | 北東アジア経済研究 |
| 巻 | 5巻 |
| 号 | 1号 |
| 資料タイプ | 紀要論文 |
| JaLCDOI | 10.18926/13303 |
| 著者 | 張 紅| |
|---|---|
| 発行日 | 2008-03-31 |
| 出版物タイトル | 北東アジア経済研究 |
| 巻 | 5巻 |
| 号 | 1号 |
| 資料タイプ | 紀要論文 |
| JaLCDOI | 10.18926/13302 |
| JaLCDOI | 10.18926/bgeou/13301 |
|---|---|
| タイトル（別表記） | Some Aspects of Influence that Difference of Language Gives to the Learning of Music |
| フルテキストURL | 131_093_099.pdf |
| 著者 | 井戸 和秀| 矢内 淑子| |
| 抄録 | 我が国では,正式に音楽教育を受けるということは,西洋音楽を学ぶということと等しい｡ それは,伝統音楽が一部導入されるようになった現在でも真実である｡特に,音楽大学や教員養成大学において,歌の学習といえば,イタリア語やドイツ語,英語等で歌うことが当然のこととなっている｡それでは,多くの日本人は,歌われる外国語の意味や歌のイメージを どのように感得しているのだろうか｡そこで,本研究では,歌を歌う際の言語の違い -ドイツ語と日本語-が聴取者に与える感得を調査した｡その結果,シューベルト作曲｢野ばら｣をドイツ語で歌った場合には,言語の意味は不明ながら,概ね軽やかでリズミックに,日本語で歌った場合には,言語の意味は漠然としながら,概ね柔らかで流れるように感得された｡ |
| キーワード | 言語の違い 歌 印象 聴取者 音楽の感得 |
| 出版物タイトル | 岡山大学教育学部研究集録 |
| 発行日 | 2006 |
| 巻 | 131巻 |
| 号 | 1号 |
| 開始ページ | 93 |
| 終了ページ | 99 |
| ISSN | 0471-4008 |
| 言語 | 日本語 |
| 論文のバージョン | publisher |
| NAID | 120002310471 |