巴伦支海大陆边缘的构造

E. Shipilov, S. Shkarubo
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引用次数: 0

摘要

研究区域的构造格局是地壳长期(约30亿年)演化的结果。许多已出版的著作和地图资料并没有专门讨论该地区的构造分区问题。东欧和北极西部平台之间的边界位置仍然是一个有争议的问题。更模糊的是,在某些情况下,对该地区构造分区的方法并不清楚。然而,这项工作建立在一个统一的理论基础上,反映了从地球动力学演化的角度解决区域构造问题的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonics of the Barents Sea Continental Edge
The tectonic situation of the studied region was formed as a result of a long (about 3 billion years) evolution of the Earth's crust. The problem of tectonic zoning of the region is not devoted to many published works and cartographic materials. The position of the borders between the East European and West Arctic platforms remains a debatable issue. More ambiguous, and in some cases, approaches to tectonic zoning of the region are not clear. Nevertheless, the work is based on a unified theoretical basis, reflecting the approach to solving the problems of regional tectonics from the perspective of geodynamic evolution.
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