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

Por um escritor misterioso
Last updated 25 março 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
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
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
Tectonic evolution of the Eocene–Oligocene Lushi Basin in the eastern Qinling belt, Central China: Insights from paleomagnetic constraints
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?, Swiss Journal of Geosciences
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
Location of the study region (black square) in central High Atlas. The
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
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Vertical-axis rotation in East Kopet Dagh, NE Iran, inferred from paleomagnetic data: oroclinal bending or complex local folding kinematics?, Swiss Journal of Geosciences
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Simplified geological map of the High Atlas with the location of the

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