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Bertotti, G. (author), Gouiza, M. (author)
Wide regions of Morocco, from the Meseta to the High Atlas, have experienced km-scale upward vertical movements during Middle Jurassic to Early Cretaceous times following the appearance of oceanic crust in the Central Atlantic. The area experiencing exhumation was flanked to the W by a domain of continuous subsidence, part of which is named the...
journal article 2012
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Gouiza, M. (author), Charton, R.J.G. (author), Bertotti, G. (author), Andriessen, P. (author), Storms, J.E.A. (author)
The Anti-Atlas belt of Morocco extends ENE–WSW, over more than 600 km, from the Atlantic margin in the west to the interior of the African plate in the east. It exhibits Precambrian rocks outcropping as basement inliers and surrounded by marine Ediacaran–Cambrian sequences around the axis of the mountain range. The belt, which has for a long...
journal article 2016
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Charton, R.J.G. (author), Bertotti, G. (author), Arantegui, Angel (author), Bulot, Luc (author)
The occurrence of km-scale exhumations during syn- and post-rift stages has been documented along Atlantic continental margins, which are also characterised by basins undergoing substantial subsidence. The relationship between the exhuming and subsiding domains is poorly understood. In this study, we reconstruct the evolution of a 50 km long...
journal article 2018
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Charton, R.J.G. (author), Bertotti, G. (author), Duval Arnould, Aude (author), Redfern, Jonathan (author), Storms, J.E.A. (author)
Continental passive margins and their hinterlands in the Atlantic realm have been the locus of many Low Temperature Thermochronology (LTT) and time-Temperature (t-T) modelling studies that evidence pre-, syn- and post-rift episodic km-scale exhumation and burial episodes. In this study, we integrate data from over 30 published LTT and t-T...
journal article 2020
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