Orogen-scale transpression accounts for GPS velocities and kinematic partitioning in the Southern Andes
Upper crustal transpression in the Southern Andes is mainly accommodated by widespread deformation on oblique-slip reverse and thrust faults, according to a comparison of scaled analogue models with the observed GPS velocity field and fault patterns.
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| Autores principales: | , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/aa955ce4e83e4049a67e4d425a81e824 |
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| Sumario: | Upper crustal transpression in the Southern Andes is mainly accommodated by widespread deformation on oblique-slip reverse and thrust faults, according to a comparison of scaled analogue models with the observed GPS velocity field and fault patterns. |
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