Pacific Plate Apparent Polar Wander, Hot Spot Fixity, and True Polar Wander During the Formation of the Hawaiian Island and Seamount Chain From an Analysis of the Skewness of Magnetic Anomaly 20r (44ᅠMa)

dc.citation.firstpage2094en_US
dc.citation.issueNumber7en_US
dc.citation.journalTitleTectonicsen_US
dc.citation.lastpage2105en_US
dc.citation.volumeNumber37en_US
dc.contributor.authorZheng, Linen_US
dc.contributor.authorGordon, Richard G.en_US
dc.contributor.authorWoodworth, Danielen_US
dc.date.accessioned2018-11-01T19:40:04Zen_US
dc.date.available2018-11-01T19:40:04Zen_US
dc.date.issued2018en_US
dc.description.abstractWhile it is well documented that the Hawaiian hot spot has shifted southward relative to the spin axis since the formation of some of the Emperor seamounts, the paleolatitude of the hot spot during the formation of the Hawaiian chain is poorly known. To better determine the latter, here we estimate the location of the 44 Ma Pacific plate paleomagnetic pole by investigating the skewness (asymmetry) of 14 airplane and 19 ship‐board crossings of magnetic anomaly 20r between the Murray and Marquesas fracture zones on the Pacific plate. The new 44 Ma paleomagnetic pole (78.0°N, 26.0°E, A95_1 = 5.4° at 101°, A95_2 = 2.0°) differs by ≈4° from its position expected if the Pacific hot spots have been fixed relative to the spin axis. This shift is independently recorded by the chron 12r (32 Ma) Pacific plate skewness paleomagnetic pole and is also confirmed by paleomagnetic poles reconstructed from the continents, indicating that global hot spots have moved in unison with respect to the spin axis, probably due to true polar wander, which may continue today as recorded by optical astronomy and geodetic very long baseline interferometry. An analysis of spreading rates recorded in the magnetic profiles indicates that spreading rates doubled between ≈50 and ≈42 Ma (confirming prior results), as expected if the bend in the Hawaiian‐Emperor chain records a change in Pacific plate motion relative to the deep mantle.en_US
dc.identifier.citationZheng, Lin, Gordon, Richard G. and Woodworth, Daniel. "Pacific Plate Apparent Polar Wander, Hot Spot Fixity, and True Polar Wander During the Formation of the Hawaiian Island and Seamount Chain From an Analysis of the Skewness of Magnetic Anomaly 20r (44ᅠMa)." <i>Tectonics,</i> 37, no. 7 (2018) Wiley: 2094-2105. https://doi.org/10.1029/2017TC004897.en_US
dc.identifier.doihttps://doi.org/10.1029/2017TC004897en_US
dc.identifier.urihttps://hdl.handle.net/1911/103283en_US
dc.language.isoengen_US
dc.publisherWileyen_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.titlePacific Plate Apparent Polar Wander, Hot Spot Fixity, and True Polar Wander During the Formation of the Hawaiian Island and Seamount Chain From an Analysis of the Skewness of Magnetic Anomaly 20r (44ᅠMa)en_US
dc.typeJournal articleen_US
dc.type.dcmiTexten_US
dc.type.publicationpublisher versionen_US
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