dc.contributor.author |
Roberts, G |
en |
dc.contributor.author |
Houghton, S |
en |
dc.contributor.author |
Underwood, C |
en |
dc.contributor.author |
Papanikolaou, I |
en |
dc.contributor.author |
Cowie, P |
en |
dc.contributor.author |
Calsteren, P |
en |
dc.contributor.author |
Wigley, T |
en |
dc.contributor.author |
Cooper, F |
en |
dc.contributor.author |
McArthur, J |
en |
dc.date.accessioned |
2014-06-06T06:49:08Z |
|
dc.date.available |
2014-06-06T06:49:08Z |
|
dc.date.issued |
2009 |
en |
dc.identifier.uri |
http://dx.doi.org/10.1029/2008JB005818 |
en |
dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/4451 |
|
dc.subject |
Strain Localization |
en |
dc.subject |
Sea Level |
en |
dc.title |
Localization of Quaternary slip rates in an active rift in 105 years: An example from central Greece constrained by 234U-230Th coral dates from uplifted paleoshorelines |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1029/2008JB005818 |
en |
heal.publicationDate |
2009 |
en |
heal.abstract |
Mapping, dating, and modeling of paleoshorelines uplifted in the footwall of the 1981 Gulf of Corinth earthquake fault, Greece (Ms 6.9–6.7), are used to assess its slip rate history relative to other normal faults in the area and study strain localization. The 234U-230Th coral ages from Cladocora caespitosa date uplifted shoreface sediments, and paleoshorelines from glacioeustatic sea level highstands at |
en |
heal.journalName |
Journal of Geophysical Research |
en |
dc.identifier.doi |
10.1029/2008JB005818 |
en |