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As mentioned in the Introduction to this volume although numerous studies of magnetic anomaly patterns in the Pacific have been made (Vine, 1966; McKenzie and Parker, 1967; Pitman and others, 1968; Herron and Hayes, 1969; Atwater and Menard, 1970; Atwater, 1970; Hayes and Pitman, 1970 and more recently Herron, in press), the analyses of the anomaly pattern of the equatorial Pacific have been limited because magnetic anomalies associated with northerly trending ridges near the equator have low amplitudes and are difficult to interpret. Consequently, very little has been published on the development of the Central Pacific some 20 degrees on either side of the equator.

An Interpretation of the Geologic History of the Eastern Equatorial Pacific from the Drilling Results of Glomar Challenger, Leg 9