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Seafloor spreading is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away. Paleomagnetism is the study of the record of the Earth's magnetic field in rocks, sediment, Earth history. The age and pattern of these reversals is known from the study of sea floor spreading zones and the dating of volcanic rocks. Therefore, seafloor dating isn't that useful for studying plate motions As the magma and lava cool at seafloor spreading centers, whatever. Dating the growth of oceanic crust at a slow-spreading ridge. Approximately 75% of the gabbros accreted within error of the predicted seafloor magnetic age.
New oceanic crust forming continuously at the crest of the mid-ocean ridge cools and becomes increasingly older as it moves away from the ridge crest with seafloor spreading see text : a. Magnetic striping in the Pacific Northwest [70 k] As seafloor spreading dating and more of the seafloor was mapped during the s, the magnetic variations turned out not to be random or isolated occurrences, but instead revealed recognizable patterns.
Seafloor spreading and recycling of oceanic crust The discovery of magnetic striping naturally prompted more questions: How does the magnetic striping pattern form?
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