Polyphased Inversions of an Intracontinental Rift: Case Study of the Marrakech High Atlas, Morocco

The High and Middle Atlas intraplate belts in Morocco correspond to Mesozoic rifted basins inverted during the Cenozoic during Africa/Eurasia convergence. The Marrakech High Atlas lies at a key location between Atlantic and Tethyan influences during the Mesozoic rifting phase but represents today hi...

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Bibliographic Details
Published in:	Tectonics (Washington, D.C.) Vol. 37; no. 3; pp. 818 - 841
Main Authors:	Leprêtre, R., Missenard, Y., Barbarand, J., Gautheron, C., Jouvie, I., Saddiqi, O.
Format:	Journal Article
Language:	English
Published:	Washington Blackwell Publishing Ltd 01.03.2018 American Geophysical Union (AGU)
Subjects:	Apatite Basins Case studies Cenozoic Convergence Cretaceous Data Deformation Earth Sciences Erosion High Atlas, intracontinental belt Inversions Jurassic low‐temperature thermochronology Magma Mesozoic Modelling Morocco Neogene Plate tectonics postrift evolution Rifting Sciences of the Universe Seismology Thermal models Morocco Africa
ISSN:	0278-7407, 1944-9194
Online Access:	Get full text
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