Tectonic Evolution of the Western High Atlas of Morocco: Oblique Convergence, Reactivation, and Transpression
The High Atlas of Morocco is a double‐vergent mountain belt developed by Cenozoic shortening and inversion of a Triassic‐Jurassic rift. The structural setting, the morphometric features, and the patterns of exhumation through time and space change remarkably both along and across the strike. Here we...
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| Published in: | Tectonics (Washington, D.C.) Vol. 39; no. 3 |
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| ISSN: | 0278-7407, 1944-9194 |
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| Abstract | The High Atlas of Morocco is a double‐vergent mountain belt developed by Cenozoic shortening and inversion of a Triassic‐Jurassic rift. The structural setting, the morphometric features, and the patterns of exhumation through time and space change remarkably both along and across the strike. Here we combine structural data with revised thermochronological data to unravel the kinematic and evolution of the western High Atlas. Our results show that the structural grain of the western High Atlas is defined by two main groups of faults, namely, thrust and oblique‐slip faults, which mainly strike subparallel from W‐E to NE‐SW. The slip direction of the thrust structures is NNW‐SSE to NW‐SE oriented, and the slip direction of the oblique‐slip faults is WSW‐ENE to NW‐SE oriented. Pieces of thermochronological and geological evidence indicate that in the last ~10 Ma the exhumation rate increased during the activity thrusts and oblique‐slip faults. The coexistence of these two fault systems also suggests partitioning of deformation under a transpressive regime. In the western High Atlas, we estimate a displacement of ~12 km on the frontal thrusts and of at least ~22 km on the axial oblique‐slip structures. Thrusts and oblique‐slip structures together result in a total cumulative displacement of ~25 km, which represents about half of the Africa‐Eurasia convergence.
Key Points
The western High Atlas builds up under a transpressional regime due to oblique convergence
Using thermochronology and fault kinematics, we infer an overall NW‐SE oriented shortening of ~25 km
The onset of the main deformation event occurred in the middle‐late Miocene |
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| AbstractList | The High Atlas of Morocco is a double‐vergent mountain belt developed by Cenozoic shortening and inversion of a Triassic‐Jurassic rift. The structural setting, the morphometric features, and the patterns of exhumation through time and space change remarkably both along and across the strike. Here we combine structural data with revised thermochronological data to unravel the kinematic and evolution of the western High Atlas. Our results show that the structural grain of the western High Atlas is defined by two main groups of faults, namely, thrust and oblique‐slip faults, which mainly strike subparallel from W‐E to NE‐SW. The slip direction of the thrust structures is NNW‐SSE to NW‐SE oriented, and the slip direction of the oblique‐slip faults is WSW‐ENE to NW‐SE oriented. Pieces of thermochronological and geological evidence indicate that in the last ~10 Ma the exhumation rate increased during the activity thrusts and oblique‐slip faults. The coexistence of these two fault systems also suggests partitioning of deformation under a transpressive regime. In the western High Atlas, we estimate a displacement of ~12 km on the frontal thrusts and of at least ~22 km on the axial oblique‐slip structures. Thrusts and oblique‐slip structures together result in a total cumulative displacement of ~25 km, which represents about half of the Africa‐Eurasia convergence.
Key Points
The western High Atlas builds up under a transpressional regime due to oblique convergence
Using thermochronology and fault kinematics, we infer an overall NW‐SE oriented shortening of ~25 km
The onset of the main deformation event occurred in the middle‐late Miocene The High Atlas of Morocco is a double‐vergent mountain belt developed by Cenozoic shortening and inversion of a Triassic‐Jurassic rift. The structural setting, the morphometric features, and the patterns of exhumation through time and space change remarkably both along and across the strike. Here we combine structural data with revised thermochronological data to unravel the kinematic and evolution of the western High Atlas. Our results show that the structural grain of the western High Atlas is defined by two main groups of faults, namely, thrust and oblique‐slip faults, which mainly strike subparallel from W‐E to NE‐SW. The slip direction of the thrust structures is NNW‐SSE to NW‐SE oriented, and the slip direction of the oblique‐slip faults is WSW‐ENE to NW‐SE oriented. Pieces of thermochronological and geological evidence indicate that in the last ~10 Ma the exhumation rate increased during the activity thrusts and oblique‐slip faults. The coexistence of these two fault systems also suggests partitioning of deformation under a transpressive regime. In the western High Atlas, we estimate a displacement of ~12 km on the frontal thrusts and of at least ~22 km on the axial oblique‐slip structures. Thrusts and oblique‐slip structures together result in a total cumulative displacement of ~25 km, which represents about half of the Africa‐Eurasia convergence. The High Atlas of Morocco is a double‐vergent mountain belt developed by Cenozoic shortening and inversion of a Triassic‐Jurassic rift. The structural setting, the morphometric features, and the patterns of exhumation through time and space change remarkably both along and across the strike. Here we combine structural data with revised thermochronological data to unravel the kinematic and evolution of the western High Atlas. Our results show that the structural grain of the western High Atlas is defined by two main groups of faults, namely, thrust and oblique‐slip faults, which mainly strike subparallel from W‐E to NE‐SW. The slip direction of the thrust structures is NNW‐SSE to NW‐SE oriented, and the slip direction of the oblique‐slip faults is WSW‐ENE to NW‐SE oriented. Pieces of thermochronological and geological evidence indicate that in the last ~10 Ma the exhumation rate increased during the activity thrusts and oblique‐slip faults. The coexistence of these two fault systems also suggests partitioning of deformation under a transpressive regime. In the western High Atlas, we estimate a displacement of ~12 km on the frontal thrusts and of at least ~22 km on the axial oblique‐slip structures. Thrusts and oblique‐slip structures together result in a total cumulative displacement of ~25 km, which represents about half of the Africa‐Eurasia convergence. The western High Atlas builds up under a transpressional regime due to oblique convergence Using thermochronology and fault kinematics, we infer an overall NW‐SE oriented shortening of ~25 km The onset of the main deformation event occurred in the middle‐late Miocene |
| Author | Lanari, R. Nahid, A. Medina, F. Youbi, N. Faccenna, C. Fellin, M. G. Essaifi, A. |
| Author_xml | – sequence: 1 givenname: R. orcidid: 0000-0002-8304-6367 surname: Lanari fullname: Lanari, R. email: riccardo.lanari@uniroma3.it organization: Roma Tre University – sequence: 2 givenname: C. orcidid: 0000-0003-0765-4165 surname: Faccenna fullname: Faccenna, C. organization: Jackson School of Geosciences, The University of Texas at Austin – sequence: 3 givenname: M. G. surname: Fellin fullname: Fellin, M. G. organization: Department of Earth Sciences – sequence: 4 givenname: A. surname: Essaifi fullname: Essaifi, A. organization: Cadi Ayyad University – sequence: 5 givenname: A. surname: Nahid fullname: Nahid, A. organization: Cadi Ayyad University – sequence: 6 givenname: F. surname: Medina fullname: Medina, F. organization: Moroccan Association of Geosciences – sequence: 7 givenname: N. surname: Youbi fullname: Youbi, N. organization: Universidade de Lisboa |
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| SubjectTerms | Cenozoic Convergence Deformation Direction Displacement Evolution Fault lines Faults Geological time Jurassic mechanical stratigraphy Morphometry strain partitioning Structures transpression Triassic Western High Atlas |
| Title | Tectonic Evolution of the Western High Atlas of Morocco: Oblique Convergence, Reactivation, and Transpression |
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