Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility
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Location of the study region (black square) in central High Atlas. The
Widespread Cretaceous secondary magnetization in the High Atlas (Morocco). A common origin for the Cretaceous remagnetizations in the western Tethys?
CCFS - Department of EPS - Faculty of Science - Macquarie University
Tethyan versus Iberian extension during the Cretaceous period in the eastern Iberian Peninsula: insights from magnetic fabrics
Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility
Geological map of Northern Morocco and location of area study (from
G.M. Sierra: M.Sc. Department of Geology, University EAFIT, Colombia, Gsierra@eafi T.edu - Co, PDF, Fault (Geology)
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
Pre‐Cenomanian vs. Cenozoic folding in the High Atlas revealed by palaeomagnetic data - Torres‐López - 2016 - Terra Nova - Wiley Online Library
SD - Report on ICDP Deep Dust workshops: probing continental climate of the late Paleozoic icehouse–greenhouse transition and beyond
Earthquake Report: Turkey! - Jay Patton online
Anisotropy of magnetic susceptibility (AMS) results by site. All
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por adulto (o preço varia de acordo com o tamanho do grupo)