Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1519
Authors: Chouliaras, G.* 
Pham, V. N.* 
Boyer, D.* 
Bernard, P.* 
Stavrakakis, G. N.* 
Title: Crustal structure of the Gulf of Corinth in Central Greece, determined from magnetotelluric soundings
Issue Date: Jan-1997
Series/Report no.: 40/1
URI: http://hdl.handle.net/2122/1519
Keywords: Magnetotelluric method
electrical properties
crustal structure earthquake
Corinth Gulf
Subject Classification04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methods 
04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy 
Abstract: The 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.
Appears in Collections:Annals of Geophysics

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