Sedimentary paleomagnetic evidence for counter-clockwise rotation of the Fiji Plateau

dc.contributor.authorGilliard, Thomas Chapman
dc.date.accessioned2015-05-22T20:02:14Z
dc.date.available2015-05-22T20:02:14Z
dc.date.issued1971
dc.descriptionTypescript.
dc.descriptionBibliography: leaves 27-28.
dc.descriptioniv, 28 leaves illustrations, map, graphs, table
dc.description.abstractThis thesis reports the results of a detailed sedimentary paleomagnetic investigation of four closely spaced 7 to 11 meter piston cores collected on the Fiji Plateau in the Western Pacific in June, 1970. The sedimentary paleomagnetic measurements reported here are important for they provide an independent means with which to test this tectonic interpretation.This thesis is also important for it is one of the first times that variations in the declination vector of marine cores have been used to deliniate the tectonic history of an oceanic crustal plate.
dc.identifier.urihttp://hdl.handle.net/10125/35995
dc.languageeng
dc.publisher[Honolulu]
dc.relationUniversity of Hawaii at Manoa [no.932]
dc.rightsAll UHM dissertations and theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission from the copyright owner.
dc.subjectPaleomagnetism -- Pacific Ocean -- Fiji Plateau
dc.subjectMarine sediments
dc.subjectSubmarine geology
dc.titleSedimentary paleomagnetic evidence for counter-clockwise rotation of the Fiji Plateau
dc.typeThesis
dc.type.dcmiText

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