Origin of the disturbed magnetic zone between the Murray and Molokai fracture zones
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference15 articles.
1. Further magnetic measurements along the Murray Fault;Raff;J. Geophys. Res.,1962
2. Magnetic anomalies over ocean ridges;Vine;Nature,1963
3. Spreading of the ocean floor: New evidence;Vine;Science,1966
4. A new class of faults and their bearing on continental drift;Wilson;Nature,1965
5. Marine magnetic anomalies, geomagnetic field reversals, and motions of the ocean floor and continents;Heirtzler;J. Geophys. Res.,1968
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1. Pacific seafloor in the 40–52 Myr old portion of the Molokai to Murray corridor;Marine Geology;2024-03
2. Elevation of Ridges and Evolution of the Central Eastern Pacific;Collected Reprint Series;2014-03-03
3. Changes in plate motions and the shape of Pacific fracture zones;Journal of Geophysical Research: Solid Earth;1996-06-10
4. Eocene propagating rifts in the southwest Pacific and their conjugate features on the Nazca Plate;Journal of Geophysical Research: Solid Earth;1991-11-10
5. Uncertainties in reconstructions of the Pacific, Farallon, Vancouver, and Kula Plates and constraints on the rigidity of the Pacific and Farallon (and Vancouver) Plates between 72 and 35 Ma;Journal of Geophysical Research;1988
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