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...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-10-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/9/1187/2018/se-9-1187-2018.pdf |