From fa6bcd3ffa263f62c9e7eebd2f00afba0c041bbd Mon Sep 17 00:00:00 2001
From: seogi_macbook <sgkang09@github.com>
Date: Thu, 11 Feb 2016 00:10:25 -0800
Subject: [PATCH] Minor changes

---
 SimPEG/Examples/EM_FDEM_SusEffects.py  |  6 ++++--
 docs/examples/EM_FDEM_1D_Inversion.rst | 26 ++++++++++++++++++++++++++
 docs/examples/EM_FDEM_SusEffects.rst   |  6 +++---
 3 files changed, 33 insertions(+), 5 deletions(-)
 create mode 100644 docs/examples/EM_FDEM_1D_Inversion.rst

diff --git a/SimPEG/Examples/EM_FDEM_SusEffects.py b/SimPEG/Examples/EM_FDEM_SusEffects.py
index b7de07bc..3e50bf91 100644
--- a/SimPEG/Examples/EM_FDEM_SusEffects.py
+++ b/SimPEG/Examples/EM_FDEM_SusEffects.py
@@ -12,7 +12,7 @@ def run(plotIt=True):
         the earth including significantly susceptible bodies (magnetite-rich rocks),
         negative data is often observed in the real part of the lowest frequency
         (e.g. Dighem system 900 Hz). This phenomenon mostly based upon magnetization
-        occurs due to a susceptible body when the magnetic field applied.
+        occurs due to a susceptible body when the magnetic field is applied.
 
         To clarify what is happening in the earth when we are exciting the earth with
         a loop source in the frequency domain we run three forward modelling:
@@ -23,7 +23,7 @@ def run(plotIt=True):
 
         We plot vector magnetic fields in the earth. For secondary fields we provide
         F[:math:`\sigma`, :math:`\mu`]-F[:math:`\sigma`, :math:`\mu_0`]. Following
-        figure show only real part, since that is our interest.
+        figure show both real and parts.
 
     """
     # Generate Cylindrical mesh
@@ -128,6 +128,7 @@ def run(plotIt=True):
             ax = [ax1, ax2, ax3]
             ax3.text(30, 50, ("Frequency=%5.2f Hz")%(frequency[ifreq]), color="k", fontsize=18)
             ax2.text(30, 50, primsec, color="k", fontsize=18)
+            ax1.text(30, 50, realimag, color="k", fontsize=18)
             for i, axtemp in enumerate(ax):
                 axtemp.plot(np.r_[0, 29.75], np.r_[-50, -50], 'w', lw=3)
 
@@ -141,6 +142,7 @@ def run(plotIt=True):
             return fig, ax
         fig1, ax1 = vizfields(1, primsec="primary", realimag="real")
         fig2, ax2 = vizfields(1, primsec="secondary", realimag="real")
+        fig4, ax4 = vizfields(1, primsec="secondary", realimag="imag")
 
 if __name__ == '__main__':
     run()
diff --git a/docs/examples/EM_FDEM_1D_Inversion.rst b/docs/examples/EM_FDEM_1D_Inversion.rst
new file mode 100644
index 00000000..acbc8cdc
--- /dev/null
+++ b/docs/examples/EM_FDEM_1D_Inversion.rst
@@ -0,0 +1,26 @@
+.. _examples_EM_FDEM_1D_Inversion:
+
+.. --------------------------------- ..
+..                                   ..
+..    THIS FILE IS AUTO GENEREATED   ..
+..                                   ..
+..    SimPEG/Examples/__init__.py    ..
+..                                   ..
+.. --------------------------------- ..
+
+
+EM: FDEM: 1D: Inversion
+=======================
+
+Here we will create and run a FDEM 1D inversion.
+
+
+
+.. plot::
+
+    from SimPEG import Examples
+    Examples.EM_FDEM_1D_Inversion.run()
+
+.. literalinclude:: ../../SimPEG/Examples/EM_FDEM_1D_Inversion.py
+    :language: python
+    :linenos:
diff --git a/docs/examples/EM_FDEM_SusEffects.rst b/docs/examples/EM_FDEM_SusEffects.rst
index 47cd3644..da4b00a0 100644
--- a/docs/examples/EM_FDEM_SusEffects.rst
+++ b/docs/examples/EM_FDEM_SusEffects.rst
@@ -9,14 +9,14 @@
 .. --------------------------------- ..
 
 
-FDEM: Effects of susceptibility
+EM: FDEM: Effects of susceptibility
 ===============================
 
 When airborne freqeuncy domain EM (AFEM) survey is flown over
 the earth including significantly susceptible bodies (magnetite-rich rocks),
 negative data is often observed in the real part of the lowest frequency
 (e.g. Dighem system 900 Hz). This phenomenon mostly based upon magnetization
-occurs due to a susceptible body when the magnetic field applied.
+occurs due to a susceptible body when the magnetic field is applied.
 
 To clarify what is happening in the earth when we are exciting the earth with
 a loop source in the frequency domain we run three forward modelling:
@@ -27,7 +27,7 @@ a loop source in the frequency domain we run three forward modelling:
 
 We plot vector magnetic fields in the earth. For secondary fields we provide
 F[:math:`\sigma`, :math:`\mu`]-F[:math:`\sigma`, :math:`\mu_0`]. Following
-figure show only real part, since that is our interest.
+figure show both real and parts.