dc.contributor.author |
Roberts, G |
en |
dc.contributor.author |
Michetti, A |
en |
dc.contributor.author |
Cowie, P |
en |
dc.contributor.author |
Morewood, N |
en |
dc.contributor.author |
Papanikolaou, I |
en |
dc.date.accessioned |
2014-06-06T06:44:54Z |
|
dc.date.available |
2014-06-06T06:44:54Z |
|
dc.date.issued |
2002 |
en |
dc.identifier.uri |
http://dx.doi.org/10.1029/2001GL013529 |
en |
dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/2145 |
|
dc.subject |
Plate Motion |
en |
dc.subject |
Plate Tectonic |
en |
dc.subject |
Seismic Hazard |
en |
dc.title |
Fault slip-rate variations during crustal-scale strain localisation, central Italy |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1029/2001GL013529 |
en |
heal.publicationDate |
2002 |
en |
heal.abstract |
Rates of plate motion are generally uniform over 10–102 Myrs timescales. Faults between tectonic plates might, therefore, be expected to show temporally-uniform slip-rates if the same number of faults remain active. For an extending region of the Eurasia-Africa plate boundary, Italy, finite throw values (vertical component of the slip) for seismogenic normal faults are less than that predicted when recent |
en |
heal.journalName |
Geophysical Research Letters |
en |
dc.identifier.doi |
10.1029/2001GL013529 |
en |