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 10 junho 2024
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
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
Anisotropy of magnetic susceptibility (AMS) results by site. All
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Evolution of the Ridges of Midelt‐Errachidia Section in the High Atlas Revealed by Paleomagnetic Data - Torres‐López - 2018 - Tectonics - Wiley Online Library
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
Paleomagnetic and magnetic fabric data from Lower Triassic redbeds of the Central Western Carpathians: new constraints on the paleogeographic and tectonic evolution of the Carpathian region
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
1 Six-steps reconstruction maps from Late Paleozoic to late Miocene
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
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility

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