Tectonic inhomogeneities of the Kristiansund—Bodø Fault Complex, offshore mid-Norway
Tectonic inhomogeneities of the Kristiansund—Bodø Fault Complex, offshore mid-Norway
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挪威中部近海克里斯蒂安松—博德断层复合体的构造不均匀性
DOI：
10.1007/978-94-009-5626-1_31
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发表时间：
1984
期刊：
影响因子：
--
通讯作者：
C. Robinson
中科院分区：
文献类型：
--
作者：
R. Gabrielsen;C. Robinson
挪威中部近海大陆架以NE-ENE-N向构造体系为主，建议将其命名为“Kristiansund-Bodø断层杂岩”。在这个体系上，叠加了一个不太明显的区域NW向构造趋势。这些断裂系统的方向走向与挪威中部陆上的平行构造走向相对应。对Kristiansund-Bodø断裂带不同部分的对比揭示了复杂的构造历史，断裂带不同部分的构造历史不同。这被认为不仅是构造事件时间差异的结果，也是各区段应力状况差异的结果。
The continental shelf offshore mid-Norway is dominated by a system of NE to ENE- and N-trending structures for which the name ‘Kristiansund-Bodø Fault Complex’ is proposed. On this system a less conspicuous regional NW structural trend is superimposed. The directional trends of these fracture systems find their counterparts in parallel structural trends onshore mid-Norway. Comparison of the different segments of the Kristiansund-Bodø Fault Complex reveals a complicated structural history, being different for the various parts of the fault complex. This is believed to be a consequence not only of difference in timing of tectonic events, but also of differences in stress situation for the segments.