1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002
Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1307
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Campo DCValoreLingua
dc.contributor.authorCAMPBELL, J.K.-
dc.date.accessioned2017-12-04T10:02:48Z-
dc.date.available2017-12-04T10:02:48Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 49-51it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/674-
dc.description.abstractTwo sites are described on transpressive faults in the eastem foothills of New Zealand's Southem Alps, where a precursor peri­od of about 200 years of accelerated downcutting and warping pre­ceded the most recent fault ruptures. Both offsets were predomi­nantly strike-slip and include a throw of about 1 metre, but base­level drop is an order of magnitude larger and extends over kilo­metre scale reaches. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectEarthquake precursor - active tectonics - fluvial geomorphology - New Zealanden
dc.titleTHE SURFACE EXPRESSION OF SLOW EARTHQUAKES?en
dc.description.pages49-51-
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