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-1309
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Campo DCValoreLingua
dc.contributor.authorCRAMPIN, S.-
dc.contributor.authorCHASTIN, S.-
dc.date.accessioned2017-12-04T10:21:02Z-
dc.date.available2017-12-04T10:21:02Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 61-62it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/676-
dc.description.abstractRecent evidence suggests that the time and magnitude of earthquakes can be stress-forecast by analysing seismic shear-wave splitting over appropriate ray paths. Theory (APE*-mode!ling) and observations demonstrate that the aspect-ratios of stress-aligned fluid-saturated grain-boundary cracks and pores are modified by the build up of stress before earthquakes. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectShear-wave velocity - seisrnic activity - transform zoneen
dc.titleTHE NEED FOR CONTROLLED-SOURCE STRESS-MONITORING SITE FOR STRESS-FORECASTING EARTHQUAKESen
dc.description.pages61-62-
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