[cig-commits] r14718 - doc/CitcomS/manual

[sue at geodynamics.org]

Author: sue
Date: 2009-04-15 12:07:23 -0700 (Wed, 15 Apr 2009)
New Revision: 14718

Modified:
   doc/CitcomS/manual/citcoms.lyx
Log:
typos fixed

Modified: doc/CitcomS/manual/citcoms.lyx
===================================================================
--- doc/CitcomS/manual/citcoms.lyx	2009-04-15 18:48:46 UTC (rev 14717)
+++ doc/CitcomS/manual/citcoms.lyx	2009-04-15 19:07:23 UTC (rev 14718)
@@ -11140,7 +11140,7 @@
 \end_inset
 
 , is 3.182.
- The total viscous heating is 7.68991, and the totoal adiabatic cooling is
+ The total viscous heating is 7.68991, and the total adiabatic cooling is
  7.71719.
  Under a steady state, these two terms should be exactly balanced.
 \end_layout
@@ -11494,6 +11494,10 @@
 \end_layout
 
 \begin_layout Standard
+
+\end_layout
+
+\begin_layout Standard
 Plate motion is imposed on top of the esolver, which has a mid-ocean ridge
  with a 5 cm/yr half-spreading rate.
  A transform fault cuts through the ridge.