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琉球是中国明、清两代的藩属国,二战前被日本吞并,改为冲绳县。二战期间,中、美、英、苏签订《开罗宣言》、《波茨坦公告》间接地对琉球处置作出原则性规定,日本以日本《投降书》的书面形式明示接受上述两国际条约。本文考察历史史实及对上述三个条约进行国际法解读,推论出日本不具有琉球主权这个结论,以正视听、扶正压邪。 相似文献
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FUMingzuo LIULejun ZHENGYanpeng LIUBaohua WUJinlong XuXiaowei 《科学通报(英文版)》2004,49(14):1512-1526
Based on an analysis of full-cover multi-beam bathymetric data, seismic and sub-bottom profiling data, and other geological-geophysical data sets, the geomorphologic features of the Ryukyu trench-arc-backarc (T-A-BA) system are delineated, and a geomorphologic map of the system is compiled. The results show that the evolution and spatial distribution patterns of the geomorphologic types of the Ryukyu T-A-BA system are controlled mainly by tectonic movements. The tectonic geomorphologic characteristics of the Ryukyu Arc (RA) differ distinctly from those of the East China Sea (ECS) continental shelf and slope. In term of geological structures, RA consists of the Tokara volcanic ridge, the Ryukyu folded ridge, the fore-arc accretion-wedge ridge and the Amami Depression and the fore-arc depressions between the ridges, which is composed of a complex of alternating island-slope ridges and fault basins. The slope of the ECS is a passive continental margin with stepwise faults. The Okinawa Trough (OT) is a backarc rift in which tectonicmovements are intensive, with active volcanic and hydro-thermal eruptions and sea floor spreading. The development of geomorphic features of the OT is controlled by the central en echelon spreading axes, the faults along the ECS slope and the marginal faults to the west of the Tokara volcanic ridge. The geomorphic complex of the OT is arranged in the following pattern: the en echelon grabens and volcanic chains formed by rifting and spreading lie in the central part of the trough, the turbidite plains incliningwards from the slope foot of the ECS lie in the westeru-northwesteru parts of the OT, and the volcaniclastic deposit plains inclining westward-northwestwards from the western slope foot of the RA lie in the easteru-southeasteru parts of the OT. In term of tectonic geomorphology, the OT forms a natural division between the sheff of the ECS and the RA. 相似文献
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LIJiabiao JINXianglong RUANAiguo WUShimin WUZiyin LIUJianhua 《科学通报(英文版)》2004,49(12):1279-1288
Based on the multibeam morpho-tectonic analysis of the Manila Trench accretionary wedge and its indentation tectonics and the contrasting researches with other geological and geophysical data, three tectonic zones of the wedge are established, faulting features, tectonic distribution and stress mechanism for the indentation tectonics are analyzed, oblique subduction along Manila Trench with convergent stress of NW55~ is presented, and the relationship of the ceasing of Eastern Subbasin spreading of South China Sea Basin to the formation of subduction zone of Manila Trench is discussed. By the model analysis and regional research, it is found that the seamount subduction along Manila Trench does not lead to the erosion of the accretionary wedge and the oblique subduction actually is a NWWtrending obduction of Luzon micro-plate that results from the NWW-trending displacement of the Philippine Sea plate. 相似文献
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吉林海沟金矿控矿构造特征及其演化 总被引:2,自引:0,他引:2
针对海沟金矿是大型石英脉型金矿床 ,矿体严格受走向NE -NNE的断裂构造控制 ,控矿构造应力作用方式有三种这一状况 ,阐述了其成矿期最大主压应力方向为NE向。说明控矿断裂构造在成矿阶段的应力处于张扭性状态 ,此应力状态有利于矿液充填、沉淀。并指出该区NE -NNE向断裂北端—海沟背斜的倾伏端是进一步工作的方向 相似文献
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5月15日,一个旨在探讨冲绳从日本独立的“琉球民族独立综合研究学会”在冲绳成立。此事提醒人们,在被日本窃据的一些列岛屿上(不局限于冲绳),曾经存在过一个千年古国——琉球王国,而琉球人民要求复活独立的呼声从未停止过。 相似文献
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日本采用三段论逻辑,“钓鱼岛属于琉球,琉球属于日本,所以钓鱼岛属于日本”,论证“日本对钓鱼岛拥有主权”。本文从国际法角度,驳斥“琉球属于日本”,论证琉球二战后已脱离日本。“钓鱼岛属于日本”的结论更是站不住脚的。二战后,美国和日本私自签订片面的双边条约私相授受琉球违反抗日盟国所签订的具有普遍约束力的多边国际条约,造成现在的琉球处于美、日两国的双重殖民地状态。即使国际社会对美、日两国以前的背信弃义、违反国际条约的行为既往不咎,将错就错,现在按照最基本的国际法《联合国宪章》,美、日两国也有义务促进琉球自治或独立。文章最后指出,琉球追求自治或独立之路充满艰辛的原因。 相似文献