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 12 abril 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
Simplified geological map of the High Atlas with the location of the
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Differential rotation in the western Sichuan-Yunnan Block and its geological implications: New palaeomagnetic evidence from the Cretaceous red beds in the southeastern margin of the Tibetan Plateau
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
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
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
Loop Pablo Calvín
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
On the ages of flood basalt events
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
Progress report of the International Geological Correlation Programme (IGCP): geoscience in the service of society
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

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