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全文: "岩船山"
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  • 石巻 良夫
    人類學雜誌
    1912年 28 巻 10 号 562-566
    発行日: 1912/11/28
    公開日: 2010/06/28
    ジャーナル フリー
  • 池谷 知彦
    電気学会誌
    2013年 133 巻 1 号 10-12
    発行日: 2013/01/01
    公開日: 2013/01/01
    ジャーナル 認証あり
  • 稲葉 充, 稲葉 かおる
    地学教育と科学運動
    2004年 47 巻 48-52
    発行日: 2004/11/30
    公開日: 2018/03/29
    ジャーナル フリー
  • 片平 忠実
    石油技術協会誌
    1969年 34 巻 6 号 314-319
    発行日: 1969/11/30
    公開日: 2008/03/27
    ジャーナル フリー
  • 稲葉 かおる
    地学教育と科学運動
    2002年 39 巻 3-10
    発行日: 2002/02/28
    公開日: 2018/03/29
    ジャーナル フリー
  • 戸祭 由美夫
    人文地理
    1972年 24 巻 2 号 129-163
    発行日: 1972/04/28
    公開日: 2009/04/28
    ジャーナル フリー
    Gôri-Sei(_??__??__??_)’is a system of local administrative division, enforced from 715 to 739-40 in the Nara era, and it consisted of two administrative divisions: ‘(_??_)’and ‘Ri(_??_)’.Up to the present only historians had pursued after this system on their historical methods. So in this paper I tried to scrutinize it on a geographical method in making reference to following primary historical materials: ‘Daizei-Sinkyû-Rekimei-Chô *in Izumo Province(_??__??__??__??__??__??__??__??__??__??_)’, ‘Daizei-Oi-Shibônin-Chô **in Bicchû Province(_??__??__??__??__??__??__??__??__??__??_)’(both in A.D. 739), ‘Izumo-no-Kuni-Fudoki ***(_??__??__??__??__??__??_)’(in A.D. 733), etc.
    Scrutiny is carried out in the below mentioned process:
    1. Presumption of the -areas in consulting documents, present names of places, etc.
    2. Presumption of the unities of Lebensräume at that time in each -areas in availing of materials such as documents, present names of places, topography, river systems, irrigation spheres of each river, remains in the Kofun era, sites of the ‘Shiki-Nai-Sha ****(_??__??__??_)’, etc.
    3. Comparison between the unities of Lebensräume and Ris in each -areas.
    Treating more than twenty cases on such method, I can clear up the four points.
    1. In nearly all -areas, several unities of Lebensräume are classified into two or three grades for their scales.
    2. Unities of Lebensräume with nearly same scale to -areas are recognized in a certain cases (Type A). On the other hand, there are not a few cases, where each unity of Lebensraum corresponds to the approximately same scale of a Ri (Type B).
    3. In the case of Type B, especially when the name of place similar to the name of Ri is found in the unity of Lebensraum with approximately same scale to that Ri, (Type B'), there is a fair possibility that the Ri was organized basing on the unity of Lebensraum. Yet even in such cases of Type B and Type B', I can hardly suppose that the Ri was always organized basing on the unity of Lebensraum.
    4. In such a case as neither in Type B nor Type B', there presents very considerable possibility that the Ri was organized almost indifferently from the unity of Lebensraum in the same -area.
    If the four above-mentioned points constitute nation-wide characteristic of the Gôri-Sei at its enforcement, it is possible to develop further inference on the basis of the results which had been already achieved by historians. Although the Gôri-Sei came in enforcement so that the government might rule over the ‘Bôko(_??__??_)’, it had been unable to meet with the actual state of affairs at that time any more than the prior system, ‘Ri-Sei(_??__??_)’ did. After a quarter of century, on the advent of new political situation, it was simply laid aside and the Gô-Sei, a not so complicated system of local administrative division as the Gôri-Sei, came close after it and kept on for hundreds of years.
    * an official document, recorded at each administrative divisions about men, women, and children, who were provided with rice from the provincial government for their old age or some other reasons.
    ** an official document, recorded at each administrative divisions about farmers who borrowed rice from the provincial government and died without repaying.
    *** ancient topographical document which the Izumo Provincial Government compiled with materials of its own territory after the order of the Central Government.
  • 岡野 裕一, 小幡 喜一, 力田 正一, 小島 正順
    地学教育と科学運動
    1997年 28 巻 19-26
    発行日: 1997/10/25
    公開日: 2018/03/29
    ジャーナル フリー
  • 中国華北地域地質見学旅行団
    地学教育と科学運動
    1993年 22 巻 117-124
    発行日: 1993/04/30
    公開日: 2018/03/29
    ジャーナル フリー
  • 堀 ひかり
    日本ジェンダー研究
    2002年 2002 巻 5 号 29-46
    発行日: 2002/09/07
    公開日: 2010/08/04
    ジャーナル フリー
  • 高尾 康太, 原 祥太郎, 桐山 毅, 橋本 彰, 金子 祥三, 泉 聡志, 酒井 信介
    日本機械学会論文集
    2014年 80 巻 820 号 TEP0366
    発行日: 2014年
    公開日: 2014/12/25
    ジャーナル フリー
    In this study, we analyze the supply-demand balance in a power system for the year 2030, utilizing an optimal power generation mix model in which the increased amount of renewable energy, high-efficiency thermal power generation, and constraint conditions that reflect realistic operation in a thermal power plant have been successfully incorporated. Our results indicate that the introduction of high-efficiency thermal power generation is capable of yielding a substantial reduction in both the annual costs involved in power generation and the annual amount of CO2 emissions. Moreover, the impact of high penetration of renewable energy on power supply operation is investigated in detail by estimating the daily capacity variation for frequency control at an interval of 15 min. Depending on the season and the weather conditions, our analysis detects that much of the time there is a capacity shortage for frequency control, which implies that high penetration of renewable energy could lead to severe integrity reduction in power operation. Finally, we discuss practical strategies for power supply operation toward resolving this capacity shortage with a particular focus on the resulting economic loss.
  • 小林 貞一
    地学雑誌
    1958年 67 巻 4 号 171-188
    発行日: 1958/12/30
    公開日: 2009/11/12
    ジャーナル フリー
    This is a critical review of the geology of the region. The stratigraphy is discussed in dividing the terrain into three tectonic units as shown in fig. 1, and schematized as indicated in the table on page 6. The best Palaeozoic sequence can be seen in the west zone. There however, the Devonian system is unknown, but present in the east flank of the Pak Lay anticline in the median zone.
    The Khorat series in the Khorat plateau in the east which contains dicotyledonous plants must be Cretaceous, instead of Jurasso-Triassic. It is quite probable for it to extend easterly into the Indosinias supérieures of South Laos which yielded Senonian Reptiles and non-marine Trigonicides faunule and southerly into Grès continentales of Cambodia which is also Upper Cretaceous, if not Palaeogene. Thus it is certain at the least that marine Jurassic and Triassic formations should be eliminated out of the continental Khorat series.
    The Triassic formation in the median zone is accompanied by eruptive rocks, like the Pahang volcanic series, but it is known paralic in North Laos. In the west zone there are Triassic and Jurassic formations devoid of volcanics. They are strongly folded, while the Cretaceous (?) red sandstone of Tenasserim is gently monoclinal.
    It is probable that the old Cimmerian folding in the median zone has confined the flooding of the Jurassic sea to the west zone and that crustal movements have taken place in the still older periods on the west side of the Indosinian massif. Nevertheless it is quite warranted that the folded mountains through the middle-west of Thailand has not been established by the Cretaceous period. Older rocks are intruded by granitic rocks, but not the Khorat series as well as the Tenasserim sandstone. They are both continental, and slightly undulated or simply inclined with low angles. Thus the vast terrain turned out land in the Palaeogene. The influence of the Himalayan orogeny was weak in this part of Asia.
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