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 26 novembro 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
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
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
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
2. Mineralogy – Petrology – Geochemistry - SWISS GEOSCIENCE
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
PDF) Plate tectonics and the intracatonic mountain ranges in Morocco – The Mesozoic – Cenozoic development of the Central High Atlas and the Middle Atlas
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
Anisotropy of magnetic susceptibility study and its significance in the Late Cretaceous-Cenozoic Sanmenxia Basin in the southeastern Shanxi rift, Central China - ScienceDirect
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 Moroccan High Atlas: A Paleomagnetic Perspective: Magnetic Techniques (Anisotropy of Magnetic Susceptibility and Intra-Plate Mountain Chain (Springer Geology): 9783031166921: Calvín, Pablo, Casas-Sainz, Antonio
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
The Geological Evolution of the Variscan Jebilet Massif, Morocco, Inferred From New Structural and Geochronological Analyses - Delchini - 2018 - Tectonics - Wiley Online Library
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Simplified geological map of the study area in the High Atlas. See
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
PDF) Application of magnetic susceptibility as a paleoclimatic proxy on Paleozoic sedimentary rocks and characterization of the magnetic signal – IGCP-580 projects and events
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High  Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Sedimentary Rock: Most Up-to-Date Encyclopedia, News & Reviews

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