Earth-prints repository, logo   DSpace

About DSpace Software
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library
Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4095

Authors: Pantosti, D.*
De Martini, P. M.*
Koukouvelas, I.*
Stamatopoulos, L.*
Palyvos, N.*
Pucci, S.*
Lemeille, F.*
Pavlides, S.*
Title: Palaeoseismological investigations of the Aigion Fault (Gulf of Corinth, Greece)
Other Titles: Tectonics
Title of journal: Comptes Rendus Geoscience
Series/Report no.: 4-5 / 336 (2004)
Publisher: Elsevier
Issue Date: Mar-2004
DOI: 10.1016/j.crte.2003.12.005
Keywords: palaeoseismology
Aigion Fault
Corinth Gulf
Greece
Abstract: We performed palaeoseismological investigations along the Aigion Fault, one of the main faults that bound the southern side of the Corinth Gulf. The mapped trace of the Aigion Fault onland is about 8 km long and may extend as much as 14 km if one includes its offshore trace. We made detailed studies at two sites adjacent to the Meganitas River. Although dating of faulted sediments was a bit problematic, we present a preliminary estimate of the faults short-term slip rate and recurrence interval. Slip rates range from 1.6 to 4.3 mmyr−1, with a maximum up to 6.3 mmyr−1. Three surface faulting events occurred in the seven centuries prior to 1888 AD, yielding an average (maximum) recurrence interval of 360 yr.
Appears in Collections:04.04.01. Earthquake geology and paleoseismology
Papers Published / Papers in press

Files in This Item:

File Description SizeFormatVisibility
CRGeo_Pantosti_2004.pdfmain article548.02 kBAdobe PDFView/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.


Share this record
Del.icio.us

Citeulike

Connotea

Facebook

Stumble it!

reddit


 

Valid XHTML 1.0! ICT Support, development & maintenance are provided by CINECA. Powered on DSpace Software. CINECA