Fix Klaver and Coath reference: 2019, not 2018.

johnrudge · Nov 22, 2021 · a66b8b2 · a66b8b2
1 parent fe6e806
commit a66b8b2
Show file tree

Hide file tree

Showing 14 changed files with 6 additions and 6 deletions.
diff --git a/README.txt b/README.txt
@@ -1,5 +1,5 @@
 The double spike toolbox
-Copyright (c) John F. Rudge 2009
+Copyright (c) John F. Rudge 2009-2021
 
 Requirements: MATLAB 7.1 (R14SP3) or higher with the Statistics and Optimization Toolboxes. It may work with older versions too, but has not been tested.
 

diff --git a/example.m b/example.m
@@ -160,7 +160,7 @@
 % mixture at a given level. When sample-limited it may be more appropriate to consider an error model
 % where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.).
 % In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'.
-% The code below recreates Figure 8 of Klaver and Coath 2018, Geostandards and Geoanalytical Research.
+% The code below recreates Figure 8 of Klaver and Coath 2019, Geostandards and Geoanalytical Research.
 isoinv = [58 60 61 62];
 spike6062 = [0.0132 0.3295 0.0014 0.6547 0.0012];
 spike6162 = [0.0109 0.0081 0.4496 0.5297 0.0017];

diff --git a/html/doublespike_product_page.html b/html/doublespike_product_page.html
@@ -465,7 +465,7 @@
 
     0.6757
 
-</pre><h2 id="20">Error model 3</h2><p>The default error model of the double spike toolbox fixes the total voltage of the beams for the overall mixture at a given level. When sample-limited it may be more appropriate to consider an error model where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.). In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'. The code below recreates Figure 8 of Klaver and Coath 2018, Geostandards and Geoanalytical Research.</p><pre class="codeinput">isoinv = [58 60 61 62];
+</pre><h2 id="20">Error model 3</h2><p>The default error model of the double spike toolbox fixes the total voltage of the beams for the overall mixture at a given level. When sample-limited it may be more appropriate to consider an error model where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.). In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'. The code below recreates Figure 8 of Klaver and Coath 2019, Geostandards and Geoanalytical Research.</p><pre class="codeinput">isoinv = [58 60 61 62];
 spike6062 = [0.0132 0.3295 0.0014 0.6547 0.0012];
 spike6162 = [0.0109 0.0081 0.4496 0.5297 0.0017];
 
@@ -644,7 +644,7 @@
 % mixture at a given level. When sample-limited it may be more appropriate to consider an error model
 % where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.).
 % In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'.
-% The code below recreates Figure 8 of Klaver and Coath 2018, Geostandards and Geoanalytical Research.
+% The code below recreates Figure 8 of Klaver and Coath 2019, Geostandards and Geoanalytical Research.
 isoinv = [58 60 61 62];
 spike6062 = [0.0132 0.3295 0.0014 0.6547 0.0012];
 spike6162 = [0.0109 0.0081 0.4496 0.5297 0.0017];

diff --git a/html/example.html b/html/example.html
@@ -465,7 +465,7 @@
 
     0.6757
 
-</pre><h2 id="20">Error model 3</h2><p>The default error model of the double spike toolbox fixes the total voltage of the beams for the overall mixture at a given level. When sample-limited it may be more appropriate to consider an error model where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.). In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'. The code below recreates Figure 8 of Klaver and Coath 2018, Geostandards and Geoanalytical Research.</p><pre class="codeinput">isoinv = [58 60 61 62];
+</pre><h2 id="20">Error model 3</h2><p>The default error model of the double spike toolbox fixes the total voltage of the beams for the overall mixture at a given level. When sample-limited it may be more appropriate to consider an error model where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.). In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'. The code below recreates Figure 8 of Klaver and Coath 2019, Geostandards and Geoanalytical Research.</p><pre class="codeinput">isoinv = [58 60 61 62];
 spike6062 = [0.0132 0.3295 0.0014 0.6547 0.0012];
 spike6162 = [0.0109 0.0081 0.4496 0.5297 0.0017];
 
@@ -644,7 +644,7 @@
 % mixture at a given level. When sample-limited it may be more appropriate to consider an error model
 % where the voltage for the sample is fixed (see John 2012, J. Anal. At. Spectrom.).
 % In the toolbox this can be achieved by changing the error model type from 'fixed-total' to 'fixed-sample'.
-% The code below recreates Figure 8 of Klaver and Coath 2018, Geostandards and Geoanalytical Research.
+% The code below recreates Figure 8 of Klaver and Coath 2019, Geostandards and Geoanalytical Research.
 isoinv = [58 60 61 62];
 spike6062 = [0.0132 0.3295 0.0014 0.6547 0.0012];
 spike6162 = [0.0109 0.0081 0.4496 0.5297 0.0017];

diff --git a/html/example.png b/html/example.png
diff --git a/html/example_01.png b/html/example_01.png
diff --git a/html/example_02.png b/html/example_02.png
diff --git a/html/example_03.png b/html/example_03.png
diff --git a/html/example_04.png b/html/example_04.png
diff --git a/html/example_05.png b/html/example_05.png
diff --git a/html/example_06.png b/html/example_06.png
diff --git a/html/example_07.png b/html/example_07.png
diff --git a/html/example_08.png b/html/example_08.png
diff --git a/html/example_09.png b/html/example_09.png