Our Earth is a layered planet with a dense iron core, a surficial crust of light rock, and between them, a solid silicate, convecting mantle. Plate tectonics is the surface manifestation of mantle convection. This activity gives rise to seafloor spreading, continental drift, earthquakes, and volcanic eruptions. Specifically, plate tectonics is the theory and study of plate formation, movement, interactions, and destruction, with seafloor spreading ridges, transform faults, and subduction zones as the plate boundaries. Today, many displaced continental blocks have been found in the world, and the original locations of some have yet to be worked out. Nevertheless, the concept of continental drift is now accepted as a necessary consequence of plate tectonics, and the complexity of mountain belts is well recognized as the product of the great mobility of lithospheric plates.
Paleomagnetism, which is the study of the ancient magnetism of the Earth, has played a central role in this...
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Zhao, X., Coe, R.S. (2007). PLATE TECTONICS, CHINA. In: Gubbins, D., Herrero-Bervera, E. (eds) Encyclopedia of Geomagnetism and Paleomagnetism. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4423-6_263
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