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Detailed File Information |
Description
This figure illustrates the periods of magnetism recorded within oceanic sediments. Magnetic polarity data is recorded at mid-ocean ridges (divergent boundaries/spreading centers) when new oceanic crust rises and begins spreading apart. |
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Geological Age Range and Timescale 5 Ma |
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Keywords magnetic anomalies, magnetic stripes, mid-ocean ridge, spreading center |
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Copyright Owner Enduring Resources for Earth Science Education (ERESE) |
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