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  • 1
    Keywords: Geology, Structural. ; Paleomagnetism. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (666 pages)
    Edition: 1st ed.
    ISBN: 9783031166938
    Series Statement: Springer Geology Series
    DDC: 538.72709644
    Language: English
    Note: Intro -- Foreword -- Preface -- Acknowledgements -- Introduction -- Contents -- Contributors -- The Geological Setting of the Moroccan High Atlas and Its Plate Tectonics Context -- 1 Geographical and Geological Setting -- 2 The High Atlas in Its Geological Context: Surrounding Geological Units -- 2.1 The Sahara Domain -- 2.2 The Anti-Atlas -- 2.3 The Meseta Domain -- 2.4 The Rif Chain -- 3 Geological Frame of the Moroccan High Atlas -- 3.1 The Atlantic High Atlas -- 3.2 The Marrakech High Atlas -- 3.3 The Central High Atlas (CHA) -- 3.4 The Eastern High Atlas -- 4 Geodynamic Frame of the High Atlas and Evolution of the APWP -- 5 The Main Geodynamic Events in North Africa: Implications in Atlasic Geology -- 5.1 Permian-Triassic Stage -- 5.2 First Rifting Event: Late Triassic to Early Jurassic -- 5.3 Second Rifting Event: Late Liassic to Early Dogger (180 Ma) -- 5.4 Bajocian-Late Jurassic Stage -- 5.5 Early Cretaceous -- 5.6 Late Cretaceous-Cenozoic Inversion -- 6 Magmatic Events, Hydrothermalism and Mineralization -- 6.1 Triassic: The CAMP Event -- 6.2 Jurassic-Cretaceous Event -- 6.3 Cenozoic Event -- 6.4 Hydrothermalism and Mineralization -- 7 Stratigraphic Frame of the Central High Atlas -- 7.1 Triassic -- 7.2 Jurassic -- 7.3 Upper Jurassic-Lower Cretaceous -- 7.4 Lower Cretaceous -- 7.5 Post-Turonian Cretaceous Deposits -- 7.6 Cenozoic Deposits -- 8 Structuring of the Moroccan High Atlas -- 8.1 Extensional Structures -- 8.2 Post-basinal, Pre-inversion Tectonic Structures -- 8.3 Alpine Compressional Structures -- 8.4 Crustal Roots for Atlasic Structures: The Geophysical Background -- 8.5 Recent Evolution of the Atlas Belt: Topographic Features -- References -- Structure of the Central High Atlas (Morocco). Constraints from Potential Field Data and 3D Models -- 1 Main Structural Features -- 1.1 Southern Atlas Fold-and-Thrust Belt (Zone 1). , 1.2 Northern Atlas Thrust System (Zone 2) -- 1.3 Western Sector: The Large Interference Synclines and Basement-Involved Folds (Demnate Area, Zone 3) -- 1.4 Central Sector (1): Thrusts and Diapiric Anticlines (La Cathédrale Area, Zone 4) -- 1.5 Central Sector (2): Thrusts, Anticlines and Diapirs (Imilchil Area, Zone 5) -- 1.6 Eastern Sector (1): Cleavage-Related Linear Structures (Tounfite Area, Zone 6) -- 1.7 Eastern Sector (2): Vergence-Switching Ridges (Midelt-Rich Area, Ziz River, Zone 7) -- 2 Seriated Cross Sections -- 3 Input from Modeling of Potential Field Data -- 3.1 Petrophysical Properties -- 3.2 Magnetic Maps Processing -- 3.3 Results -- 3.4 The Geophysical Anomalies in Their Relation to Geological Features and Evolution of the CHA -- 3.5 2.5D Modelling. Configuration and Interpretation of Magnetic and Gravimetric Models -- 4 Contributions of 3-D Reconstructions to the Geometry of the Central High Atlas -- 4.1 Methods and Workflow -- 4.2 3D Structural Model of the Central High Atlas -- 4.3 Potential and Limitations of the 3D Model -- References -- Magnetic Properties of the Jurassic Sedimentary Rocks of the Central High Atlas Affected by a Regional Chemical Remagnetization -- 1 Methodology -- 2 General Magnetic Fraction in the Atlasic Rocks -- 2.1 Carbonates -- 2.2 Red Beds -- 3 Magnetic Properties of Magnetite-Bearing Remagnetized Carbonates -- 3.1 SP vs. SSD Grain Size -- 3.2 ARM vs. IRM Experiments -- 3.3 Coercivity Spectra -- 3.4 Discussion and Summary -- 4 Carriers of the Magnetic Susceptibility -- 4.1 Magnetic Susceptibility of Carbonates -- 4.2 Magnetic Susceptibility of Red-Beds -- References -- Paleomagnetism of the Central High Atlas. The Widespread Cretaceous Remagnetization and Structural Implications -- 1 Materials, Sampling Strategy and Methods -- 2 Natural Remanent Magnetization of Mesozoic High Atlas Rocks -- 2.1 Carbonates. , 2.2 Red Beds -- 3 Directional Analysis of the Characteristic Remanent Magnetization -- 4 Age of the High Atlas Remagnetization -- 5 Extent of the High Atlas Carbonate Remagnetization -- 6 Restoration of the Paleomagnetic Directions. Paleo-Dips at the Remagnetization Acquisition Time (100 Ma) -- 6.1 Method -- 6.2 Paleo-dip Evolution Diagram (PED) -- 7 Conclusions -- Appendix -- References -- Geodynamic Evolution During the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility -- 1 Sampling and Methodology -- 2 Magnetic Fabric (RT-AMS) Results -- 2.1 Global RT-AMS Results -- 2.2 RT-AMS by Zones and Types -- 3 Magnetic Subfabrics (LT-AMS and AARM) Results -- 3.1 Scalar Parameters -- 3.2 Orientation Distribution of Grains, Information of the Magnetic Subfabrics (LT-, RT-AMS and AARM) -- 3.3 Comparison with Petrofabrics -- 4 Structural Interpretation of the Magnetic Fabrics/Tectonic Implications of the Magnetic Fabric Orientation -- 4.1 Strain Characterization from Magnetic Fabrics in the Central High Atlas -- 4.2 Timing of Acquisition of AMS: Information Derived from Magnetic Subfabrics Separation -- 5 Conclusions -- Appendix -- References -- Kinematics of Structures and Basin Evolution in the Central High Atlas. Constraints from AMS and Paleomagnetic Data -- 1 Paleodips and Fold Tests. Results and Limitations -- 2 Origin of Individual Structures According to Paleomagnetism and Magnetic Fabrics Data -- 3 Restored Cross-Sections -- 4 Significance and Meaning of Major Structures in the Central High Atlas from the Perspective of Magnetic Techniques -- 4.1 Deformation of the Paleozoic Basement -- 4.2 The Asymmetry of the Chain: Compressional Features of the Southern Atlas Fold-and-Thrust Belt -- 4.3 Compressional Features of the Northern Belt -- 4.4 Diapirism, Magmatism and Thrusting in the Central High Atlas. , 4.5 Geophysical Constraints to Large-Scale Structural Features -- 4.6 Internal Deformation: The Cleavage Domain -- 4.7 The Structural Style of the Central Zone: Thin-Skinned or Thick Tectonics? -- 4.8 Geometry of the Overall Extension and Inversion of the Atlasic Basin -- 5 Conclusions. The Contribution of Magnetic Techniques to the Evolution of the Central High Atlas -- 5.1 Paleomagnetism and AMS Applied to the Study of the CHA -- 5.2 The Intermediate Stage in Basin Evolution -- 5.3 Basin Geometry: Transtension Versus Salt Tectonics? -- 5.4 Final Considerations: Comparison with Other Basins of the Tethys Domain -- 5.5 Concluding Remarks -- Appendix -- References.
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  • 2
    Keywords: Geology. ; Sedimentology. ; Geodynamics. ; Hoher Atlas ; Gesteinsmagnetismus ; Paläomagnetismus ; Magnetische Suszeptibilität ; Tektonik ; Orogenese ; Hoher Atlas ; Paläotektonik ; Geologisches Profil ; Geologie ; Tektogenese
    Description / Table of Contents: The geological setting of the Moroccan High Atlas and its plate tectonics context -- Structure of the Central High Atlas (Morocco). Constraints from potential field data and 3D models -- Magnetic properties of the remagnetized carbonates of the Central High Atlas (Morocco) -- Paleomagnetism of the Central High Atlas. The widespread Cretaceous Remagnetization and structural implications -- Geodynamic evolution during the Mesozoic and Cenozoic in the Central High Atlas of Morocco from Anisotropy of Magnetic Susceptibility -- Kinematics of structures and basin evolution in the Central High Atlas. Constraints from AMS and paleomagnetic data.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXII, 646 p. 324 illus., 311 illus. in color.)
    Edition: 1st ed. 2023.
    ISBN: 9783031166938
    Series Statement: Springer Geology
    Language: English
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  • 3
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    Springer
    In:  In: The Geology of Iberia: A Geodynamic Approach Volume 3: The Alpine Cycle. , ed. by Quesada, C. and Oliveira, J. T. Springer, Cham, pp. 487-505. ISBN 978-3-030-11294-3
    Publication Date: 2020-01-07
    Description: The Alpine orogeny is well recorded onshore and offshore by tectonic inversion of the Mesozoic rift basins. Large scale linear seamounts (more than 250 km long and with up to 5 km of uplift) involving oceanic and continental lithosphere were carried on top of thrusts, such as the Gorringe seamount and the Estremadura Spur in the SouthWest and West Iberia Margin, respectively. The SouthWest Iberia Margin also recorded the westward migration of the Gibraltar Oceanic slab as the westwards propagation of the Neo-Tethys subduction. Rotation of the tectonic compression from NW-SE to WNW-ESE inPliocene times caused the development of large scale dextral wrench faults as the present day Africa-Iberia plate boundary. Neotectonics of this plate boundary caused large to mega-scale destructive earthquakes and tsunamis.
    Type: Book chapter , NonPeerReviewed
    Format: text
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