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Grand Banks Abyssal Plain
Linked via "geomagnetic reversal timescales"
Magnetic Polarity Chronology
Analysis of deep-sea cores reveals a clear correlation between the magnetic inclination within the sediments and established geomagnetic reversal timescales. The average magnetic signature suggests significant deposition during the Gauss Normal chron.
| Magnetic Polarity Chron | Time Span (Ma) | Characteristic Location | Average Magnetic Intensity (nT) |