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Thermal stresses at the oceanic-continental margin
dc.contributor.authorPollack, Henry N.en_US
dc.date.accessioned2006-04-17T16:12:18Z
dc.date.available2006-04-17T16:12:18Z
dc.date.issued1967-03en_US
dc.identifier.citationPollack, Henry N. (1967/03)."Thermal stresses at the oceanic-continental margin." Earth and Planetary Science Letters 2(2): 116-118. <http://hdl.handle.net/2027.42/33354>en_US
dc.identifier.urihttp://www.sciencedirect.com/science/article/B6V61-473FM1T-C0/2/b4f4ff1260cf84a173f6fca200ed7a7een_US
dc.identifier.urihttps://hdl.handle.net/2027.42/33354
dc.description.abstractDissimilar temperature profiles beneath oceans and continents give rise to thermoelastic stresses at and adjacent to the oceanic-continental margin. Computations of the magnitude and orientation of the maximum shear stress field reveal a zone of shear dipping beneath the continent from the margin.en_US
dc.format.extent231635 bytes
dc.format.extent3118 bytes
dc.format.mimetypeapplication/pdf
dc.format.mimetypetext/plain
dc.language.isoen_US
dc.publisherElsevieren_US
dc.titleThermal stresses at the oceanic-continental marginen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelGeology and Earth Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.contributor.affiliationumDepartment of Geology and Mineralogy, and Geophysics Laboratory, The University of Michigan, Ann Arbor, Michigan, USAen_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/33354/1/0000752.pdfen_US
dc.identifier.doihttp://dx.doi.org/10.1016/0012-821X(67)90111-2en_US
dc.identifier.sourceEarth and Planetary Science Lettersen_US
dc.owningcollnameInterdisciplinary and Peer-Reviewed


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