Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility

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Last updated 21 fevereiro 2025
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
SD - Report on ICDP Deep Dust workshops: probing continental climate of the late Paleozoic icehouse–greenhouse transition and beyond
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
G.M. Sierra: M.Sc. Department of Geology, University EAFIT, Colombia, Gsierra@eafi T.edu - Co, PDF, Fault (Geology)
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Progress report of the International Geological Correlation Programme (IGCP)
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Full article: Paleocurrent and paleowind direction reconstruction research progress and perspectives: a review
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Geological map of Northern Morocco and location of area study (from
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Widespread Cretaceous secondary magnetization in the High Atlas (Morocco). A common origin for the Cretaceous remagnetizations in the western Tethys?
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Tethyan versus Iberian extension during the Cretaceous period in the eastern Iberian Peninsula: insights from magnetic fabrics
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Sketch map of Mesozoic rifting along the northern African margin and
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Applying magnetic techniques to determine the evolution of reactive diapirs: A case study of the Lusitanian basin - ScienceDirect
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Triassic magmatism in the European Southern Alps as an early phase of Pangea break-up, Geological Magazine
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Widespread Cretaceous secondary magnetization in the High Atlas (Morocco). A common origin for the Cretaceous remagnetizations in the western Tethys?

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