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The Seafloor High Issue in Article 76 of the LOS Convention: Some Views from the Perspective of Legal Interpretation

机译:《 LOS公约》第76条中的海底高位问题:法律解释的一些观点

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摘要

The three categories of the seafloor highs provided for in Article 76 of the 1982 United Nations Convention on the Law of the Sea should be interpreted from the legal perspective and in light of the principle of the natural prolongation. "Oceanic ridges of the deep ocean floor," which are not part of the natural prolongation of the land territory of the coastal state, are the submarine features that have no geomorphological continuity with the landmass of the coastal state. "Submarine elevations," which are not only part of the natural prolongation of the land territory of the coastal state but also the natural component of the continental margin, are those submarine features that have geomorphological as well as geological continuity with the landmass of the coastal state. "Submarine ridges," which are part of the natural prolongation of the land territory of the coastal state but not the natural component of the continental margin, are those submarine features that have geomorphological continuity with the landmass of the coastal state. There are some clear trends as well as obvious variances in the practice of the Commission on the Limits of the Continental Shelf in this regard.
机译:1982年《联合国海洋法公约》第七十六条规定的三类海底高度应从法律角度并根据自然延伸原则加以解释。并非沿海国土地领土自然延伸的一部分的“深海底洋脊”是与沿海国陆地没有地貌连续性的海底特征。那些“海底高程”不仅是沿海国土地领土自然延伸的一部分,而且是大陆边缘的自然组成部分,是那些与沿海海陆具有地貌和地质连续性的海底特征州。这些“海底脊”是沿海国土地领土自然延伸的一部分,但不是大陆边缘的自然组成部分,是与沿海国陆体具有地貌学连续性的那些海底特征。在这方面,大陆架界限委员会的做法存在明显趋势,也存在明显差异。

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