4.4 Article

Geochemistry and Petrogenesis of Lower Jurassic Mafic Rock Suites in the External Rif Belt, and Chemical Geodynamics of the Central Atlantic Magmatic Province (CAMP) in Northwest Morocco

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Summary: The chaotic rock units in the Northern Apennines and Western Alps, representing Jurassic ophiolites, were influenced by tectonic deformation and high-pressure metamorphism during formation, leading to debates on their lithostratigraphic position. A comparative analysis of these units revealed the nature of processes involved in their formation and suggested that they can be used as proxies for identifying metamorphosed counterparts. The sedimentological processes associated with slow-spreading MOR tectonics and accretionary prism development were found to contribute to sediment budgets, indicating uniform and synchronous processes in the formation of Jurassic oceanic lithosphere in the LPOB.

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