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Oblique rifting: the rule, not the exception
<p>Movements of tectonic plates often induce oblique deformation at divergent plate boundaries. This is in striking contrast with traditional conceptual models of rifting and rifted margin formation, which often assume 2-D deformation where the rift velocity is oriented perpendicular to th...
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| 主要な著者: | , , |
|---|---|
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Copernicus Publications
2018-10-01
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| シリーズ: | Solid Earth |
| オンライン･アクセス: | https://www.solid-earth.net/9/1187/2018/se-9-1187-2018.pdf |
| タグ: |
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