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Estimation of the potential type of faulting in relation to the stress field: the North Aegean case study

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dc.contributor.author Chiotis, ED en
dc.contributor.author Tsoutrelis, CE en
dc.date.accessioned 2014-03-01T01:08:47Z
dc.date.available 2014-03-01T01:08:47Z
dc.date.issued 1992 en
dc.identifier.issn 0191-8141 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/10696
dc.subject Case Study en
dc.subject Stress Field en
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.other Geophysics en
dc.subject.other Rock--Stresses en
dc.subject.other Seismology--Aegean Sea en
dc.subject.other Deviatoric Stress Ratio en
dc.subject.other Geological Faults en
dc.subject.other Geology en
dc.subject.other fault reactivation en
dc.subject.other faulting en
dc.subject.other focal mechanism en
dc.subject.other stress field en
dc.subject.other Aegean Sea en
dc.title Estimation of the potential type of faulting in relation to the stress field: the North Aegean case study en
heal.type journalArticle en
heal.identifier.primary 10.1016/0191-8141(92)90058-5 en
heal.identifier.secondary http://dx.doi.org/10.1016/0191-8141(92)90058-5 en
heal.language English en
heal.publicationDate 1992 en
heal.abstract The relation between the angle of slip during fault reactivation and the applied stress field is investigated through a plot of the deviatoric stress ratio r = (sigma(V) - sigma(h)/(sigma(H) - sigma(h)) vs the fault strike direction measured from sigma(H), assuming that one of the principal stresses, sigma(V), is vertical. This approach is applied to the North Aegean trough fault zone on the basis of neotectonic data presented previously by other authors, and conclusions are drawn as to the potential type of faulting along the trough since late Miocene. The same reasoning is also applied to earthquake focal mechanisms of the Northern Aegean region. en
heal.publisher PERGAMON-ELSEVIER SCIENCE LTD en
heal.journalName Journal of Structural Geology en
dc.identifier.doi 10.1016/0191-8141(92)90058-5 en
dc.identifier.isi ISI:A1992HE96900008 en
dc.identifier.volume 14 en
dc.identifier.issue 2 en
dc.identifier.spage 215 en
dc.identifier.epage 223 en


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