对北冰洋外大陆架界限的一些法律和科学认识的评述

Jongseong Ryu, V. Kaczynski
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引用次数: 1

摘要

在外大陆架划界的标准中,最具争议的是《联合国海洋法公约》第76条的海脊规定。2001年,俄罗斯宣称对北冰洋中部大陆架拥有主权。本文以俄罗斯向大陆架界限委员会(CLCS)提交的意见书为重点,旨在广泛探讨大陆架的历史、法律和科学方面,这些方面对于寻求在其200海里(M)领土之外主张延伸大陆架的沿海国来说是必要的。具有自然延伸标准的山脊规定可以作为一种有用的工具来调用,以消除350米对大陆边缘外部界限的限制。要对脊进行正确的分类,应仔细考虑三个特征:地质连续性、地壳中性和大陆坡脚的包络性。在准备向CLCS提交的材料时,应仔细考虑地貌数据以及地质和地球物理数据。中大陆委在审查沿海国提交的文件时,有充分责任解释这些条款,并适用法律和科学标准。鉴于中大陆架仲裁委员会工作量大,很容易被驳回,沿海国应花费相当多的时间和精力,以海脊和自然延伸为基础主张大陆架外部界限。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Review on some aspects of legal and scientific understandings regarding outer continental shelf limits in the Arctic Ocean
Among the most controversial criteria in the delimitation of outer continental shelf are ridge provisions in article 76 of the United Nations Convention on the Law of the Sea. In 2001, Russia claimed its sovereign rights to the continental shelf in central Arctic Ocean. Focusing on this Russian submission to the Commission on the Limits of the Continental Shelf (CLCS), this article aims to widely address the historical, legal and scientific aspects of the continental shelf that are necessary to be reviewed by coastal States seeking to claim the extended continental shelf beyond their 200 nautical miles (M) territory. Ridge provisions with the natural prolongation standard can be invoked as a useful tool in order to remove the 350 M constraints for outer limits of the continental margin. Three features should be carefully considered to classify ridges correctly: geological continuity, crustal neutrality and envelop of the foot of the continental slope. Geomorphological data ought to be carefully considered together with geological and geophysical data to prepare the submission to the CLCS. The CLCS has a full responsibility to interpret the provisions and apply the legal and scientific criteria in reviewing the submission by coastal States. Given the high possibility of getting easily rejected due to the heavy workload of the CLCS, a coastal State should expend considerable amounts of time and efforts in claiming its outer limit of continental shelf based on a ridge and natural prolongation.
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