dc.contributor.author |
Walker, J |
en |
dc.contributor.author |
Roberts, G |
en |
dc.contributor.author |
Cowie, P |
en |
dc.contributor.author |
Papanikolaou, I |
en |
dc.contributor.author |
Sammonds, P |
en |
dc.contributor.author |
Michetti, A |
en |
dc.contributor.author |
Phillips, R |
en |
dc.date.accessioned |
2014-06-06T06:49:07Z |
|
dc.date.available |
2014-06-06T06:49:07Z |
|
dc.date.issued |
2009 |
en |
dc.identifier.uri |
http://dx.doi.org/10.1016/j.jsg.2009.06.011 |
en |
dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/4446 |
|
dc.subject |
Landscape Evolution |
en |
dc.subject |
Late Pleistocene |
en |
dc.subject |
Seismic Hazard |
en |
dc.subject |
Strain Rate |
en |
dc.title |
Horizontal strain-rates and throw-rates across breached relay zones, central Italy: Implications for the preservation of throw deficits at points of normal fault linkage |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/j.jsg.2009.06.011 |
en |
heal.publicationDate |
2009 |
en |
heal.abstract |
In order to investigate the relationship between the throws and 3D orientation of breaching faults crossing relay zones, kinematic data, throw-rates and total throws have been measured for an active normal fault in the Italian Apennines that displays a relay zone at its centre. The c. 0.8km long breaching fault dips at 67±5° and strikes obliquely to c. 2–3km long |
en |
heal.journalName |
Journal of Structural Geology |
en |
dc.identifier.doi |
10.1016/j.jsg.2009.06.011 |
en |