Reworked the header of each org-mode file
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@@ -41,6 +41,7 @@ For all the measurements shown here:
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:END:
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<<sec:effect_control_all>>
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** ZIP file containing the data and matlab files :ignore:
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#+begin_src bash :exports none :results none
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if [ matlab/effect_control_all.m -nt data/effect_control_all.zip ]; then
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cp matlab/effect_control_all.m effect_control_all.m;
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@@ -366,6 +367,7 @@ First, we compute the Power Spectral Density of the signals coming from the Geop
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:END:
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<<sec:effect_control_one>>
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** ZIP file containing the data and matlab files :ignore:
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#+begin_src bash :exports none :results none
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if [ matlab/effect_control_one.m -nt data/effect_control_one.zip ]; then
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cp matlab/effect_control_one.m effect_control_one.m;
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@@ -634,6 +636,7 @@ And we compare the Amplitude Spectral Densities (figures [[fig:psd_marble_comp_l
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:END:
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<<sec:effect_symetrie_driver>>
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** ZIP file containing the data and matlab files :ignore:
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#+begin_src bash :exports none :results none
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if [ matlab/effect_symetrie_driver.m -nt data/effect_symetrie_driver.zip ]; then
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cp matlab/effect_symetrie_driver.m effect_symetrie_driver.m;
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@@ -784,6 +787,7 @@ First, we compute the Power Spectral Density of the signals coming from the Geop
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:END:
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<<sec:tf_stages_geophone>>
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** ZIP file containing the data and matlab files :ignore:
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#+begin_src bash :exports none :results none
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if [ matlab/tf_stages_geophone.m -nt data/tf_stages_geophone.zip ]; then
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cp matlab/tf_stages_geophone.m tf_stages_geophone.m;
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