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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1519
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dc.contributor.authorallChouliaras, G.; National Observatory of Athens, Institute of Geodynamics, Athens, Greeceen
dc.contributor.authorallPham, V. N.; Institut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, Franceen
dc.contributor.authorallBoyer, D.; Institut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, Franceen
dc.contributor.authorallBernard, P.; Institut de Physique du Globe de Paris, Dèpartement de Seismologie, Paris, Franceen
dc.contributor.authorallStavrakakis, G. N.; National Observatory of Athens, Institute of Geodynamics, Athens, Greeceen
dc.date.accessioned2006-09-11T07:47:27Zen
dc.date.available2006-09-11T07:47:27Zen
dc.date.issued1997-01en
dc.identifier.urihttp://hdl.handle.net/2122/1519en
dc.description.abstractThe magnetotelluric sounding method at 15 sites was employed to investigate the electrical properties of the crust and upper mantle near the epicentral region of the June 15 1995, Ms = 6.1, destructive earthquake in the Gulf of Corinth, Central Greece. The magnetotelluric results indicate the presence of a conductive zone in the mid-crust at a depth of 9 to 12 km near the seismogenetic region. The existence of this zone with a thickness of around 7 km can be explained by the presence of fluids in a zone of ductile shear. A second electrical discontinuity was also found at a depth of about 28 km and this may well correspond to the Moho below the Gulf of Corinth.en
dc.format.extent1968297 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries1/40 (1997)en
dc.subjectMagnetotelluric methoden
dc.subjectelectrical propertiesen
dc.subjectcrustal structure earthquakeen
dc.subjectCorinth Gulfen
dc.titleCrustal structure of the Gulf of Corinth in Central Greece, determined from magnetotelluric soundingsen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methodsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorChouliaras, G.en
dc.contributor.authorPham, V. N.en
dc.contributor.authorBoyer, D.en
dc.contributor.authorBernard, P.en
dc.contributor.authorStavrakakis, G. N.en
dc.contributor.departmentNational Observatory of Athens, Institute of Geodynamics, Athens, Greeceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, Franceen
dc.contributor.departmentInstitut de Physique du Globe de Paris, Dèpartement de Seismologie, Paris, Franceen
dc.contributor.departmentNational Observatory of Athens, Institute of Geodynamics, Athens, Greeceen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptNational Observatory of Athens, Institute of Geodynamics, Athens, Greece-
crisitem.author.deptInstitut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, France-
crisitem.author.deptInstitut de Physique du Globe de Paris, Laboratoire de Geomagnetisme, Paris, France-
crisitem.author.deptInstitut de Physique du Globe de Paris, Dèpartement de Seismologie, Paris, France-
crisitem.author.deptNational Observatory of Athens, Institute of Geodynamics, Athens, Greece-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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