From Oblique Thrust to Strike-Slip Fault: Progressive Stages of an Accretionary Wedge Development
Accretionary wedges of orogenic belts develop differently based on the direction of thrusting, which can be perpendicular to oblique to the belt. In the case of oblique thrusting, stress partitioning occurs, which dissects the accretionary wedge, changes the tectonic regime from thrusting to strike-...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , , , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
GeoScienceWorld
2025-04-01
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| Rangatū: | Lithosphere |
| Urunga tuihono: | https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/doi/10.2113/2024/lithosphere_2024_182/654093/lithosphere_2024_182.pdf |
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