Late Jurassic magnetic polarity sequence

Polarity reversal sequences have been observed in the Brushy Basin Member of the Morrison Formation (Upper Jurassic, Kimmeridgian-Tithonian age) at two sites in western Colorado separated by 80 km. The two polarity reversal sequences display a good correlation of relative lengths and number of polarity intervals and thus may provide a significant correlation tool in this laterally variable formation.The whole polarity sequence observed in the Morrison Formation correlates very well with the oldest portion of lineated anomalies of the sea floor. The sedimentary record on land and the anomaly pattern of the oceanic crust both show the same relative lengths and approximate number of polarity intervals, as well as ratio of reversed to normal polarity.