Changeset 3016

Timestamp:

May 30, 2006, 12:08:03 PM (19 years ago)

Author:

sexton

Message:

fixups

Location:

production/onslow_2006/report

Files:

• introduction.tex (modified) (2 diffs)
• onslow_2006_report.tex (modified) (1 diff)
• tsunami_scenario.tex (modified) (1 diff)

production/onslow_2006/report/introduction.tex

@@ -6 +6 @@
 coastline to tsunamigenic earthquakes originating from 
 the Sunda Arc subduction zone. There is
-historic evidence of such events, \bibitem{CB:ausgeo}, 
+historic evidence of such events, \cite{CB:ausgeo}, 
 and FESA has sought to assess
 the relative risk of its urban and regional communities to the tsunami
@@ -24 +24 @@
 ANUGA has been developed by GA and the Australian National University
 (ANU) to solve the nonlinear shallow water
-wave equation using the finite volume technique (described in \cite{ON:modsim}).
+wave equation using the finite volume technique 
+(described in \cite{ON:modsim}).
 An advantage of this technique is that the cell resolution can be changed
 according to areas of interest and that wetting and drying

production/onslow_2006/report/onslow_2006_report.tex

@@ -121 +121 @@
      
    \section{References}
+   \input{references}
 
    \section{Metadata}

production/onslow_2006/report/tsunami_scenario.tex

@@ -2 +2 @@
 to develop the preliminary tsunami hazard assessment which 
 was delivered to FESA in September 2005,
-\bibitem{CB:FESA}. In that assessment, a suite of
+\cite{BC:FESA}. In that assessment, a suite of
 tsunami were evenly spaced along the Sunda Arc subduction zone and there
 was no consideration of likelihood. Other sources were not considered, such