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Scientists have utilized radiometric dating techniques, particularly through the analysis of ancient rocks and minerals, to determine when plate tectonics began. By dating the oldest oceanic crust and continental rocks, researchers have established a timeline that suggests plate tectonics began around 3 billion years ago. Additionally, geological evidence, such as the formation of specific rock types and the alignment of ancient magnetic fields, supports this timeline by indicating the movement of tectonic plates over geological time.

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