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Paleomagnetism is the study of the fossil magnetism in rocks. It has been paramount in determining that the continents have drifted over the surface of the Earth throughout geological time. The fossil magnetism preserved in the ocean floor has demonstrated how continental drift takes place through the process of sea-floor spreading. The methods and techniques used in paleomagnetic studies of continental rocks and of the ocean floor are described and then applied to determining horizontal movements of the Earth's crust over geological time. An up-to-date review of global paleomagnetic data enab

Magnetisme [Paleo] --- Magnetostratigraphy --- Magnétisme [Paléo] --- Paleomagnetics --- Paleomagnetism --- Paleomagnetisme --- Paléomagnetisme --- Plaattektoniek --- Plaques [Tectonique des ] --- Plate tectonics --- Remanent magnetism --- Tectonics [Plate ] --- Tectonique des plaques --- Tektoniek ]Plaat] --- Paleomagnetism. --- Plate Tectonics. --- Plate tectonics. --- Tectonics, Plate --- Geodynamics --- Palaeomagnetism --- Geomagnetism

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Continental Red Beds

Red beds. --- Issue --- Sedimentary rocks. --- Rocks, Sedimentary --- Rocks --- Beds, Red --- Red rock --- Redbeds --- Sedimentary rocks --- SEDIMENTOLOGIE --- DEPOTS MILIEUX MIXTES --- SEDIMENTOLOGIE DEPOTS CONTINENTAUX --- PETROLOGIE ROCHES SEDIMENTAIRES --- ROCHES FERRUGINEUSES ET MANGANESIFERES --- DIAGENESE ET METASOMATOSE --- GEOPHYSIQUE --- GEOMAGNETISME --- PALEOMAGNETISME