Pacific plate deformation from horizontal thermal contraction

Simple item page
dc.citation.journalTitleGeologyen_US
dc.contributor.authorKreemer, Cornéen_US
dc.contributor.authorGordon, Richard G.en_US
dc.contributor.orgEarth, Environmental and Planetary Sciencesen_US
dc.date.accessioned2014-09-09T16:04:20Zen_US
dc.date.available2014-09-09T16:04:20Zen_US
dc.date.issued2014en_US
dc.description.abstractThe central approximation of plate tectonics is that the plates are rigid, which gives the theory its rigor and predictive power. Space geodetic measurements are consistent with the rigidity of stable plate interiors, but some failures of plate-circuit closure, in particular of oceanic plates, indicate that plates may be measurably non-rigid. We explore the hypothesis that horizontal thermal contraction causes deformation of oceanic plates. Here we show significant expected displacement fields due to thermal contraction for the Pacific plate based on a previously proposed relationship between sea-floor age and strain rate and on two end-member assumptions on how strain compatibility is enforced. The predicted maximum 2.2 mm/yr southeastward motion of the north-eastern part of the plate relative to the Pacific-Antarctic Rise may contribute to a large part of the non-closure of the Pacific-North America plate motion circuit. Our predicted displacement rates cannot (yet) be confirmed by current space-geodetic data and will require seafloor geodesy with 1 mm/yr accuracy. The spatial distribution of predicted moment rate agrees reasonably well with that of intraplate earthquakes epicenters, similar to what is observed for plate boundary zones. Our results suggest that plate-scale horizontal thermal contraction is significant and that it may be partly released seismically.en_US
dc.identifier.citationKreemer, Corné and Gordon, Richard G.. "Pacific plate deformation from horizontal thermal contraction." <i>Geology,</i> (2014) Geological Society of America: http://dx.doi.org/10.1130/G35874.1.en_US
dc.identifier.doihttp://dx.doi.org/10.1130/G35874.1en_US
dc.identifier.urihttps://hdl.handle.net/1911/77150en_US
dc.language.isoengen_US
dc.publisherGeological Society of Americaen_US
dc.rightsThis is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by the Geological Society of America.en_US
dc.titlePacific plate deformation from horizontal thermal contractionen_US
dc.typeJournal articleen_US
dc.type.dcmiTexten_US
dc.type.publicationpost-printen_US
Files
Original bundle
Now showing 1 - 1 of 1
Thumbnail Image
Name:
G35874-Kreemer-final.pdf
Size:
157.15 KB
Format:
Adobe Portable Document Format
Description:
Download
Collections
Faculty Publications