When did the Moroccan High Atlas Mountains get high? Constraints on neo- and active tectonics from fluvial geomorphology and palaeoaltimetry

Authors

SJ Boulton, School of Geography, Earth and Environmental Sciences
M Stokes, School of Geography, Earth and Environmental Sciences
J Vandevelde
AE Mather, School of Geography, Earth and Environmental Sciences

ORCID

• SJ Boulton: 0000-0002-8251-0025
• M Stokes: 0000-0003-3788-4615
• AE Mather: 0000-0001-6634-8681

DOI Link

10.13140/RG.2.1.2352.2805

Publication Date

2016-06-03

Event

7th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology

Publication Title

Proceedings of the 7th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology (J.P. McCalpin & C. Gruetzner, eds.).

Acceptance Date

2016-04-06

Recommended Citation

Boulton, S., Stokes, M., Vandevelde, J., & Mather, A. (2016) 'When did the Moroccan High Atlas Mountains get high? Constraints on neo- and active tectonics from fluvial geomorphology and palaeoaltimetry', Proceedings of the 7th International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology (J.P. McCalpin & C. Gruetzner, eds.)., . Available at: 10.13140/RG.2.1.2352.2805