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Article: INTERPRETATION OF THE CRUSTAL STRESS FIELD IN NORTHEAST NORTH AMERICA.

TitleINTERPRETATION OF THE CRUSTAL STRESS FIELD IN NORTHEAST NORTH AMERICA.
Authors
Lee, CFAsmis, HW
Issue Date1979
Citation
U.S. Symposium On Rock Mechanics, 1979, p. 655-662 How to Cite?
AbstractThe following factors are discussed: the effects of the Earth's rotation on the development of longitudinal and latitudinal stresses in crustal rocks; the potential relationship between plate tectonics, Chandler wobble, changes in speed of rotation, and earthquakes; and continental glaciation (and erosion) as a causative mechanism for the buildup of residual stresses.
Persistent Identifierhttp://hdl.handle.net/10722/175553
ISSN
0085-574X

 

DC FieldValueLanguage
dc.contributor.authorLee, CFen_US
dc.contributor.authorAsmis, HWen_US
dc.date.accessioned2012-11-26T08:59:40Z-
dc.date.available2012-11-26T08:59:40Z-
dc.date.issued1979en_US
dc.identifier.citationU.S. Symposium On Rock Mechanics, 1979, p. 655-662en_US
dc.identifier.issn0085-574Xen_US
dc.identifier.urihttp://hdl.handle.net/10722/175553-
dc.description.abstractThe following factors are discussed: the effects of the Earth's rotation on the development of longitudinal and latitudinal stresses in crustal rocks; the potential relationship between plate tectonics, Chandler wobble, changes in speed of rotation, and earthquakes; and continental glaciation (and erosion) as a causative mechanism for the buildup of residual stresses.en_US
dc.languageengen_US
dc.relation.ispartofU.S. Symposium on Rock Mechanicsen_US
dc.titleINTERPRETATION OF THE CRUSTAL STRESS FIELD IN NORTHEAST NORTH AMERICA.en_US
dc.typeArticleen_US
dc.identifier.emailLee, CF: leecf@hkucc.hku.hken_US
dc.identifier.authorityLee, CF=rp00139en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0018551157en_US
dc.identifier.spage655en_US
dc.identifier.epage662en_US
dc.identifier.scopusauthoridLee, CF=8068602600en_US
dc.identifier.scopusauthoridAsmis, HW=6602602933en_US
dc.identifier.issnl0085-574X-

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