Thermal stresses at the oceanic-continental margin
dc.contributor.author | Pollack, Henry N. | en_US |
dc.date.accessioned | 2006-04-17T16:12:18Z | |
dc.date.available | 2006-04-17T16:12:18Z | |
dc.date.issued | 1967-03 | en_US |
dc.identifier.citation | Pollack, 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.uri | http://www.sciencedirect.com/science/article/B6V61-473FM1T-C0/2/b4f4ff1260cf84a173f6fca200ed7a7e | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/33354 | |
dc.description.abstract | Dissimilar 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.extent | 231635 bytes | |
dc.format.extent | 3118 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Elsevier | en_US |
dc.title | Thermal stresses at the oceanic-continental margin | en_US |
dc.type | Article | en_US |
dc.rights.robots | IndexNoFollow | en_US |
dc.subject.hlbsecondlevel | Geology and Earth Sciences | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Geology and Mineralogy, and Geophysics Laboratory, The University of Michigan, Ann Arbor, Michigan, USA | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/33354/1/0000752.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1016/0012-821X(67)90111-2 | en_US |
dc.identifier.source | Earth and Planetary Science Letters | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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