Magnetic Lineations on the Flanks of the Marquesas Swell: Implications for the Age of the Seafloor
Document Type
Article
Publication Date
6-1988
Digital Object Identifier (DOI)
https://doi.org/10.1029/GL015i006p00573
Abstract
Four magnetic anomaly profiles across the Marquesas swell were obtained on the Crossgrain expedition of the R/V Thomas Washington in April 1987. The data cover a poorly dated region of the Pacific between the Galapagos and Marquesas fracture zones. Magnetic lineations trending approximately 350° in the vicinity of the swell were identified as anomalies 20 through 29, differing from identifications proposed by previous workers. Our identifications imply that the seafloor beneath the Marquesas Islands formed at a half-spreading rate of approximately 40-45 mm/yr during Paleocene and early Eocene time (65 to 50 Ma). The offset across the Marquesas fracture zone apparently increased from approximately 700 to 850 km between the times of anomalies 21 and 13.
Rights Information
Was this content written or created while at USF?
No
Citation / Publisher Attribution
Geophysical Research Letters, v. 15, issue 6, p. 573-576
Scholar Commons Citation
Kruse, Sarah, "Magnetic Lineations on the Flanks of the Marquesas Swell: Implications for the Age of the Seafloor" (1988). School of Geosciences Faculty and Staff Publications. 946.
https://digitalcommons.usf.edu/geo_facpub/946
