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 abril 2025


SE - What can seismic noise tell us about the Alpine reactivation of the Iberian Massif? An example in the Iberian Central System

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
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

Synthetic stratigraphic column of the central and eastern High Atlas

a) Location sketch map of the Atlas Mountains in the Western

CCFS - Department of EPS - Faculty of Science - Macquarie University

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

Anisotropy of magnetic susceptibility study and its significance in the Late Cretaceous-Cenozoic Sanmenxia Basin in the southeastern Shanxi rift, Central China - ScienceDirect
G.M. Sierra: M.Sc. Department of Geology, University EAFIT, Colombia, Gsierra@eafi T.edu - Co, PDF, Fault (Geology)

Geological map of Northern Morocco and location of area study (from

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

Evolution of the Ridges of Midelt‐Errachidia Section in the High Atlas Revealed by Paleomagnetic Data - Torres‐López - 2018 - Tectonics - Wiley Online Library
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