Continent-ocean transition at the western Barents Sea/Svalbard continental margin
Continent-ocean transition at the western Barents Sea/Svalbard continental margin
复制标题
西巴伦支海/斯瓦尔巴群岛大陆边缘的大陆-海洋过渡
DOI：
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发表时间：
1987
期刊：
影响因子：
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通讯作者：
A. Myhre
中科院分区：
文献类型：
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作者：
O. Eldholm;J. Faleide;A. Myhre
The change in crustal type at the western Barents Sea/Svalbard margin takes place over a narrow zone related to primary rift and shear structures reflecting the stepwise opening of the Greenland Sea. Regionally, the margin is composed of two large shear zones and a central rifted-margin segment. Local transtension and transpression at the plate boundary caused the early Cenozoic tectonism in Svalbard and the western Barents Sea, and might explain the prominent marginal gravity and velocity anomalies.
