南海諸島不僅擁有豐富的資源，更處於重要的戰略位置，目前共有六個主要 聲索國主張對南海諸島擁有領土主權，分別是中華民國、中國大陸、菲律賓、越 南、馬來西亞與汶萊，美國雖然不是聲索國，但基於維護其在南海的重要利益， 所以也涉入南海的紛爭，這使得南海的局勢更加複雜。 我國、中國大陸與菲律賓皆主張對南海諸島中的黃岩島享有主權，2012 年中 國大陸與菲律賓之間爆發了黃岩島事件，更使南海的緊張情勢升至最高，於是菲 律賓便訴諸於國際仲裁法庭，仲裁庭並未就主權的歸屬作出判決，而是對《聯合 國海洋法公約》的解釋問題作出裁判，但南海諸島的主權爭奪仍就方興未艾。 有關領土主權的取得，1928 年帕瑪斯島案的仲裁法官指出「持續與和平展示 領土主權幾乎就等於主權本身」，而這便是「有效統治」的核心，本文因此挑選 四個與有效統治高度相關的國際司法機構判決來作分析，並參酌相關國際法的原 則與發展，以歸納出「有效統治」的構成要件、衡量指標與法律效果，並利用這 個歸納結果來對我國、中國大陸與菲律賓在黃岩島領土主權的爭端進行分析，判 斷結果雖是我國擁有黃岩島的領土主權，但由於我國目前沒有實質控制該島礁， 因此本文也試著提出具體建議來強化我國的主張。 / The islands of the South China Sea (SCS) not only have an abundance of resources, but also are strategically located. There are six major countries that claim territorial sovereignty over the islands, including the R.O.C. (Taiwan), Mainland China, the Philippines, Vietnam, Malaysia and Brunei. Although the U.S.A. is not one of the claimants, it is still involved in the SCS dispute because of its important interests in that region. Thus, the situation in the SCS has become more complicated. Taiwan, Mainland China, and the Philippines all claim to have sovereignty over Huangyen Island in the SCS. The “Huangyen Island Incident” between Mainland China and the Philippines broke out in 2012, bringing tensions in SCS to a height. The Philippines thus resorted to the international Arbitral Tribunal. The tribunal didn’t make a ruling on sovereignty, but it made a ruling regarding the explanatory question of the United Nations Convention on the Law of the Sea. However, the tit-for-tat over the sovereignty of the SCS islands continues. Regarding the acquisition of territorial sovereignty, the arbitrator of the 1928 Palmas case indicated that, “the continuous and peaceful display of territorial sovereignty is as good as a title.” This is the exact the core of effectivités. To conclude the components, indicators and the legal effect of the effectivités, the thesis thus considered related principals and development of international law, and selected four rulings of international judicial bodies to analyze, as these four ruling are highly-relevant to effectivités. Furthermore, based on the results of the above analysis, this thesis also analyzes the territorial sovereignty dispute over Huangyen Island among Taiwan, Mainland China, and the Philippines. The analysis concludes that Taiwan has the territorial sovereignty over Huangyen Island. Given the fact that Taiwan doesn't substantially control it, the thesis also tries to come up with advice to strengthen Taiwan’s claim.

京都大学 / 0048 / 新制・論文博士 / 博士(農学) / 乙第12938号 / 論農博第2818号 / 新制||農||1034(附属図書館) / 学位論文||H27||N4897(農学部図書室) / 32148 / 名古屋大学生命農学研究科生物圏資源学専攻 / (主査)教授 水山 高久, 教授 柴田 昌三, 教授 谷 誠 / 学位規則第4条第2項該当 / Doctor of Agricultural Science / Kyoto University / DFAM

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第21060号 / 工博第4424号 / 新制||工||1687(附属図書館) / 京都大学大学院工学研究科都市社会工学専攻 / (主査)教授 角 哲也, 教授 藤田 正治, 准教授 竹門 康弘 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM

京都大学 / 0048 / 新制・論文博士 / 博士(文学) / 乙第13152号 / 論文博第639号 / 新制||文||661(附属図書館) / 京都大学大学院文学研究科思想文化学専攻 / (主査)教授 根立 研介, 教授 横田 冬彦, 教授 平川 佳世 / 学位規則第4条第2項該当 / Doctor of Letters / Kyoto University / DGAM

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第21307号 / 工博第4505号 / 新制||工||1701(附属図書館) / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 小池 克明, 教授 石田 毅, 准教授 塚田 和彦 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DGAM

日本基督教団の戦後の宣教における社会的関与の史的研究。「宣教の社会的関与」「宣教の霊性」という概念モデルによって一群の宣教者に関して論究する。社会的関与における宣教は教団教会の内外双方向で福音の現実化を問い、また生起させていると指摘する。 / 博士(神学) / Doctor of Theology / 同志社大学 / Doshisha University

2001年5月29日第11次《聯合國海洋法公約》締約國會議通過SPLOS/72號決定，於1999年5月13日以前對其生效之公約締約國，如欲依《聯合國海洋法公約》第76條規定主張200海里以外之大陸礁層，必須在1999年5月13日起算10年內向聯合國大陸礁層界限委員會提交與其所主張大陸礁層外部界限相關科學及技術佐證資料。由於《聯合國海洋法公約》所定義之大陸礁層外部界限範圍可能超越專屬經濟海域範圍，而大陸礁層不僅是魚類資源較豐富也是漁業活動重要資源地，同時也是海底油氣與礦場等重要自然資源的集中地區。因此，包括我國相鄰之日本、菲律賓、越南、馬來西亞等公約締約國紛紛進行大陸礁層調查來擴展自己國家的海洋權益。至2009年12月止，已有51個延伸大陸礁層外部界限之提案，及44個初步資訊，聯合國大陸礁層界限委員會並已就部分提案作成決議。 日本於2008年11月12日向聯合國大陸礁層界限委員會提出該國延伸大陸礁層外部界限之申請，卻也因此引起中國大陸及韓國對日本提案中以「沖之鳥礁」為基礎劃定超出200海里延伸大陸礁層之主張提出反對意見，質疑「沖之鳥礁」之法律地位及其所能享有的海域管轄空間。本論文爰由《聯合國海洋法公約》第121條「島嶼制度」形成的過程、相關國家實踐及學者見解，以及《聯合國海洋法公約》中「大陸礁層」之相關規範及聯合國大陸礁層界限委員會之組織與運作情形，探討日本的延伸大陸礁層外部界限提案中以「沖之鳥礁」為基礎主張延伸大陸礁層之適法性問題，並分析以聯合國大陸礁層界限委員會作為「沖之鳥礁」法律地位爭端解決途徑之可能性等。研究結果顯示，日本提案以「沖之鳥礁」為基礎主張延伸大陸礁層外部界限不符合《聯合國海洋法公約》第121條第3項規定，但該項規定並未具備有習慣國際法的效力，亦缺乏客觀的認定標準，聯合國大陸礁層界限委員會的場域無法解決「沖之鳥礁」的法律地位爭端，其他沿海國僅能利用聯合國大陸礁層界限委員會中「第三國意見」之機制凸顯爭端的存在，提醒國際社會注意此類島礁的海域管轄空間主張的合理性問題，並應尊重公約所賦予的權利與義務。 / On 29 May 2001, the 11th Meeting of States Parties to the United Nations Convention on the Law of the Sea (UNCLOS) adopted the SPLOS/72 Decision regarding the date of commencement of the ten-year period for making submissions to the Commission on the Limits of the Continental Shelf set out in Article 4 of Annex II to the UNCLOS. It was decided that, in the case of a State Party for which the Convention entered into force before 13 May 1999, the ten-year time period for it to submit the scientific and technical data supporting the outer limits of its continental shelf beyond 200 nautical miles under Article 76 of the UNCLOS shall be taken to have commenced on 13 May 1999. For quite a few States the outer limits of their continental shelf as defined by the UNCLOS may go beyond the limits of the Exclusive Economic Zone (EEZ). Besides, continental shelf is abundant in fisheries resources, crude oil, natural gas and minerals. Consequently, the neighboring States of Taiwan, including Japan, the Philippines, Viet Nam, and Malaysia, have already begun their surveys on continental shelf in order to expand their interests hidden in the ocean. As of December of 2009, there have been 51 formal submissions and 44 Preliminary Information delivered to the United Nations. The Commission on the Limits of the Continental Shelf (CLCS) has been undertaking the consideration of these submissions and already completed such process for some of them with recommendations. For Japan, the submission to support the outer limits of its extended continental shelf was made on 12 November 2008 to the CLCS. Such submission was challenged by China and Korea whose focus is on the part of extended continental shelf generated by Oki-no-tori Shima. The legal status of Oki-no-tori Shima as being capable of generating EEZ, continental shelf, and extended continental shelf beyond 200 nautical miles, is being disputed by the communications from China and Korea. To provide educated comments on such controversy, this thesis will discuss the legislative process of Article 121 of the UNCLOS, namely, the regime of islands. Related state practices and teachings of the most highly qualified publicists will be studied in this connection. The author will also examine the regime of continental shelf under the UNCLOS and the institution of the CLCS. These will pave the way to scrutinize the legality of using Oki-no-tori Shima as the basis to generate extended continental shelf as having been done by Japan in its submission. The author will also explore the feasibility for the CLCS to settle the dispute over the legality of Japanese submission with respect to Oki-no-tori Shima. As shown by research works, the Japanese submission using Oki-no-tori Shima to generate extended continental shelf is inconsistent with Article 121(3) of the UNCLOS. However, the rule as contained in Article 121(3) has not yet been received into customary international law. Also lacking are the objective criteria to decide whether a given rock meets the conditions as stipulated by Article 121(3) or not. The forum of the CLCS is not suitable to settle the dispute over the legality of using Oki-no-tori Shima by Japan to generate extended continental shelf. Other coastal States can only use the forum of the CLCS to demonstrate the legal controversy over this case through sending third party communications to notify the CLCS the existence of dispute and their unwillingness to support the CLCS to consider the Japanese submission with respect to the part of Oki-no-tori Shima. As submitted by this author, the international community should be reminded of the necessity to respect the integrity of the rights and duties enshrined by the UNCLOS. Also worthy of careful scrutiny is the legitimacy of such kinds of exaggerated maritime claims generated by the rock as defined by Article 121(3) of the UNCLOS.

科学研究費補助金 研究種目:国際学術研究 課題番号:06045017 研究代表者:鈴木 和博 研究期間:1994-1995年度

The Chachahuén volcanic complex, with the Cerro Bayo laccolith as one of the largest intrusions, is part of back-arc Payenia volcanic province in western central Argentina. Laccoliths show potential for generating oil in sedimentary basins and producing ore deposits. It is crucial to put more effort into understanding the magma plumbing system beneath the Chachahuén volcanic complex, which the Cerro Bayo laccolith is part of. Thus this project present the first thermobarometric modelling for the Cerro Bayo laccolith and the Chachahuén volcanic complex. Several thermometers and barometers were applied to plagioclase, amphibole and clinopyroxene to understand magma evolution in the underlying plumbing system. The dacitic to rhyodacitic laccolith rocks from Cerro Bayo have porphyric textures with plagioclase in the form of both clots (glomerocrysts) and single crystals, amphibole and clinopyroxene as main phenocrysts, while enclaves are more mafic in composition and have equigranular textures. Plagioclase in the sample varies from andesine to labradorite with a composition of An22-An68, while the clinopyroxene can be classified into diopside to augite with cores (Mg#=76-84) and rims (Mg#62-72). Amphibole, varies from pargasite, ferropargasite to magesiohastingsite and hastingsite, which can be grouped into three groups according to the Mg#: low Mg# amphibole (Mg# = 40-51), medium Mg# amphibole (Mg# = 52-61) and high Mg# amphibole (Mg# = 62-78). Besides, most of the Fe-Ti oxides in the samples are titanomagnetite with Usp mol.% in the range of 0.04-0.54. Results from clinopyroxene-liquid thermobarometers suggest a crystallization depth of 44 to 51 km for clinopyroxene cores and a crystallization depth of 19 to 31 km for rims, of which the derived crystallization temperatures are in the range of 1144 to 1170 °C and 973 to 1002 °C respectively. On the other hand, different thermobarometers of amphibole give consistent results of crystallization temperatures and depths. According to the amphibole-liquid thermometer, low Mg# (Mg#= 40-51) amphiboles have the lowest crystallization temperature in the range of 898 to 931°C, while medium Mg# (Mg#=52-61) amphiboles have higher crystallization temperatures in the range of 951 to 972°C and high Mg# (Mg# = 62-78) amphiboles have highest crystallization temperatures between 991 and 1013°C. The depth translated from pressure derived from amphibole-liquid barometers give a shallower crystallization depth range from 19 to 30 km for low Mg# amphiboles, a deeper crystallization depth in the range of 22 to 39 km for high Mg# amphiboles and deepest crystallization depth range of 27 to 41 km for medium Mg# amphiboles. Moreover, a depth from 2 to 20 km could be gained from the plagioclase-liquid thermobarometry which crystallized at 883 to 910°C. It is worth to point out that crystallization depth of clinopyroxene cores is deeper than the Moho in the Chachahuén area, while crystallization depth and temperatures of clinopyroxene rims are consistent with those of high Mg# amphiboles. Consistent temperatures and depths are also found for crystallization of plagioclase and low Mg# amphiboles which intergrow with each other. Thus, a multi-level magma plumbing system began from below the Moho, with a mushy zone in the upper crust, could be suggested to exist beneath the Cerro Bayo laccolith. Evidence from both petrology and geochemistry also indicate fractional crystallization as well as processes of magma mixing and recharge during magma evolution. / Chachahuén火山综合体，包含其最大的侵入体Cerro Bayo岩盘，是位于阿根廷中西部Payenia弧后火山区的一部分。前人研究多着重于岩石学、地球化学和地层学方面，因而针对下伏岩浆涌升系统的研究在该地区极具前瞻性，需要投入更多工作。本文首次尝试对Chachahuén火山复合体应用温压计进行研究，针对斜长石、角闪石和单斜辉石应用了不同的温度计和压力计，以揭示下伏于Cerro Bayo岩盘的岩浆涌升系统中的岩浆演化。 来自Chachahuén火山复合体Cerro Bayo岩盘的英安质-流纹英安质火成岩具有板状-似斑状结构，其斑晶主要为单晶或聚合物形式存在的斜长石、角闪石及单斜辉石。此外，岩盘中还发现具等粒结构的酸性捕虏体的存在。样品中斜长石（An=22-68）主要成分为中长石至拉长石.单斜辉石主要为透辉石和普通辉石，常发育高镁值核部（Mg#=76-84）和低镁值环带（Mg#62-72）。角闪石主要为韭闪石、铁韭闪石、镁绿钙闪石和绿钙闪石，可根据镁值进一步划分为三个组：低镁值组（Mg# = 40-51），低镁值组（Mg# = 52-61）和高镁值组（Mg# = 62-71）。此外，样品中的钛铁氧化物重要为钛磁铁矿（Usp%=0.04-0.54）。 单斜辉石-熔体温压计的结果表明单斜辉石的核部和环带的结晶温度和深度有所差异：核部具有较高的结晶温度（1144-1170 °C）和较深的结晶深度（44-50km），而环带具有较低的结晶温度（973-1002 °C）和较浅的结晶深度（18-31 km）。与角闪石相关的不同温压计给出了类似的结晶温度和压力，其中存在的微小差异均在误差范围内。因此本文将角闪石-熔体温压计的结果作为最终结果，其显示低镁值角闪石具有较低结晶温度（898-931°C），中镁值角闪石具较高结晶温度（951-972°C），而髙镁值角闪石具最高结晶温度（991-1013°C）。角闪石的结晶深度特征有所不同：低镁值角闪石的结晶深度最浅（19-30km），髙镁值角闪石的结晶深度较深（22-39 km），反而中镁值角闪石结晶深度最深（27-41 km）。斜长石-熔体温压计给出的斜长石结晶温度和深度分别为883-910°C及1-20km。 值得一提的是单斜辉石核部的结晶深度位于研究区莫霍面之下。同时，单斜辉石的环带与髙镁值角闪石具有相似的结晶温度和深度，而斜长石及共生的低镁值角闪石具有相似的结晶温度。因此可以推测，Cerro Bayo岩盘之下，发育一个自莫霍面之下开始的多层岩浆上涌系统。而岩石学和地球化学的证据还表明在岩浆发育过程中岩浆分化结晶和岩浆重注和混合作用并存。 / En lakkolit är en grund magmaficka och en vanligt förekommande del av en vulkan, vilken kan bilda en länk mellan djupa magmatiska aktiviteter och vulkanutbrott. Forskning om kompositionen och bildandet av grunda magmafickor kan hjälpa till att öka förståelsen om geologiska faror och naturresurser. Vid Cerro Bayo exponeras en grund magmakammare vilken utgör en del av Chachahuén vulkankomplexet i Argentina. Det här projektet fokuserar på det magmatiska lagringssystemet och magmautvecklingen vid Cerro Bayo. Magmasammansättningen och magmakammarens förhållanden såsom tryck, temperatur och vattenhalt samt vattensystemets struktur är viktiga faktorer som styr magmatiska processer. För att förstå magmautvecklingen under Cerro Bayo inleddes projektet med en kompositionsanalys av bergprover och mineral. Därefter genomfördes termobarometrisk modellering för att bestämma temperatur- och tryckförhållandena för kristalliseringen av mineraler i det magmatiska systemet. Resultaten av modelleringen tyder på att ett magmatiskt rörsystem av flera nivåer existerar under Cerro Bayo lakkoliten. Det djupaste magmamagasinet ligger på 44-50 km och når upp till 22-41 km i nedre jordskorpan, medan de grunda reservoarerna av magma ligger på ett djup av 2-20 km i övre jordskorpan som slutligen når den grunda magmafickan. Vidare indikerar analysen av mineralstruktur och mineralkemi processer av fraktionerad kristallisering samt påfyllning och blandning av magma under magmautvecklingen. Magman genomgick fraktionerad kristallisering under rörelser uppåt från de djupaste magmakammarna. Magmans temperatur varierar från högre än 1100 ° C till ~ 900 ° C. Ansamlingar av magma fortsatte att fylla på magmamagasin i nedre och övre jordskorpan. Blandning av magma inträffade när en ansamling varmare magma rörde sig från nedre till övre jordskorpreservoarer och påverkade såväl migrering av magma som placeringen av Cerro Bayo lakkoliten

京都大学 / 0048 / 新制・課程博士 / 博士(工学) / 甲第18238号 / 工博第3830号 / 新制||工||1587(附属図書館) / 31096 / 京都大学大学院工学研究科社会基盤工学専攻 / (主査)教授 三ｹ田 均, 教授 朝倉 俊弘, 教授 清野 純史 / 学位規則第4条第1項該当 / Doctor of Philosophy (Engineering) / Kyoto University / DFAM