The Paleomagnetic Significance of Aeromagnetic Surveys of the Hawaiian Islands

dc.contributor.author Malahoff, Alexander
dc.contributor.author Strange, William E.
dc.date.accessioned 2009-09-01T03:14:16Z
dc.date.available 2009-09-01T03:14:16Z
dc.date.issued 1965-07
dc.description.abstract Aeromagnetic surveys of the Hawaiian Islands have revealed that the primary magnetic anomalies associated with the islands are dipole anomalies caused by the intrusive rocks of the volcanic centers and rift zones. Comparisons of the direction of magnetization indicated by the dipole anomalies with results of laboratory measurements on lavas show that in many cases the lavas possess reverse polarization while the intrusive rocks are normally polarized. These results must be taken into account when interpreting the magnetic field of submerged marine volcanic features such as seamounts and when establishing periods of reversal in the earth's magnetic field.
dc.identifier.citation Malahoff A, Strange WE. 1965. The paleomagnetic significance of aeromagnetic surveys of the Hawaiian Islands. Pac Sci 19(3): 390-392.
dc.identifier.issn 0030-8870
dc.identifier.uri http://hdl.handle.net/10125/10766
dc.language.iso en-US
dc.publisher University of Hawai'i Press
dc.title The Paleomagnetic Significance of Aeromagnetic Surveys of the Hawaiian Islands
dc.type Article
dc.type.dcmi Text
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