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-...
محفوظ في:
| المؤلفون الرئيسيون: | , , , , , , , , , , , , , |
|---|---|
| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
GeoScienceWorld
2025-04-01
|
| سلاسل: | Lithosphere |
| الوصول للمادة أونلاين: | https://pubs.geoscienceworld.org/gsa/lithosphere/article-pdf/doi/10.2113/2024/lithosphere_2024_182/654093/lithosphere_2024_182.pdf |
| الوسوم: |
لا توجد وسوم, كن أول من يضع وسما على هذه التسجيلة!
|