| dc.contributor.author |
Papanikolaou, I |
en |
| dc.contributor.author |
Papanikolaou, D |
en |
| dc.date.accessioned |
2014-06-06T06:47:33Z |
|
| dc.date.available |
2014-06-06T06:47:33Z |
|
| dc.date.issued |
2007 |
en |
| dc.identifier.uri |
http://dx.doi.org/10.1016/j.quaint.2007.03.020 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/3674 |
|
| dc.subject |
Active Fault |
en |
| dc.subject |
Seismic Hazard |
en |
| dc.subject |
Seismic Reflection |
en |
| dc.subject |
Shear Zone |
en |
| dc.title |
Seismic hazard scenarios from the longest geologically constrained active fault of the Aegean |
en |
| heal.type |
journalArticle |
en |
| heal.identifier.primary |
10.1016/j.quaint.2007.03.020 |
en |
| heal.publicationDate |
2007 |
en |
| heal.abstract |
Several seismic hazard scenarios are examined concerning the seismic potential of the North Aegean Basin (NAB), based for the first time purely on geological data. Detailed analysis of the bathymetry incorporated by seismic reflection profiling has recently revealed the neotectonic structure of the NAB and demonstrates that the dominant structure is a 160km long NE–SW trending fault, comprising of four |
en |
| heal.journalName |
Quaternary International |
en |
| dc.identifier.doi |
10.1016/j.quaint.2007.03.020 |
en |