Skip to content

fix fieldstone manual latex compilation. #5

New issue

Have a question about this project? Sign up for a free GitHub account to open an issue and contact its maintainers and the community.

Sign up for GitHub

By clicking “Sign up for GitHub”, you agree to our terms of service and privacy statement. We’ll occasionally send you account related emails.

Already on GitHub? Sign in to your account

Open
MFraters wants to merge 1 commit into
base: master
Choose a base branch
from
Open

fix fieldstone manual latex compilation. #5

Show file tree
Hide file tree
Changes from all commits
Commits
Show all changes
1 commit
Select commit
File filter

Filter by extension

Filter by extension
Conversations
Failed to load comments.
Loading
Jump to
Jump to file
Failed to load files.
Loading
Diff view
Diff view
4 changes: 2 additions & 2 deletions gravity.tex
View file
Open in desktop
Original file line number Diff line number Diff line change
Expand Up @@ -207,10 +207,10 @@
\textrm{for} \; l=0,1,2,3,... \; \textrm{and} \; m=-l,-l+1,...,l-1,l
\label{eq:spha5}
\end{equation}
The phase factor (−1) , introduced originally by Condon and Shortley, is convenient for
The phase factor (-1) , introduced originally by Condon and Shortley, is convenient for
applications in quantum mechanics. Note that eq. (\ref{eq:spha4}) implies that
\[
Y_l^{−m} (\theta, \phi) = (−1)^m Y_l^m (\theta,\phi)^∗
Y_l^{-m} (\theta, \phi) = (-1)^m Y_l^m (\theta,\phi)^*
\]
where the star means complex conjugation.

Expand Down
2 changes: 1 addition & 1 deletion oldies.tex
View file
Open in desktop
Original file line number Diff line number Diff line change
Expand Up @@ -131,7 +131,7 @@

\begin{center}
\includegraphics[height=6cm]{images/history/nesb99}\\
{\captionfont 1989: Model geometry, boundary conditions and 3-D ¢nite element mesh used in
{\captionfont 1989: Model geometry, boundary conditions and 3-D finite element mesh used in
the calculations. The circles denote a free-slip condition. The arrow denotes the velocity
applied in some calculations to the southern boundary of the Tyrrhenian domain to simulate
the motion of the African plate. The springs represent the buoyant restoring force applied
Expand Down
2 changes: 1 addition & 1 deletion python_codes/fieldstone_59/text.tex
View file
Open in desktop
Original file line number Diff line number Diff line change
Expand Up @@ -127,7 +127,7 @@
$p$ is the grain size exponent, $Q$ is the activation energy for the creep
mechanism at stake (J$\cdot$mol$^{-1}$ ), $p$ is the hydrostatic pressure (MPa),
$V$ the activation volume (m$^3\cdot$mol$^{-1}$),
$R$ is the gas constant (J$\cdot$K$^{−1}\cdot$mol$^{-1}$), and $T$ the absolute temperature (K).
$R$ is the gas constant (J$\cdot$K$^{-1}\cdot$mol$^{-1}$), and $T$ the absolute temperature (K).
The effect of $pV$ is assumed to be very small \cite{dust01}
and is ignored for the remainder of this work.

Expand Down
4 changes: 2 additions & 2 deletions python_codes/gravity_01/text.tex
View file
Open in desktop
Original file line number Diff line number Diff line change
Expand Up @@ -10,7 +10,7 @@
The horizontal spacing between nodes is $hx$ and the vertical spacing is $hy$.

\begin{center}
\includegraphics[width=7cm]{/home/cedrict/Desktop/FIELDSTONE/fieldstone/python_codes/gravity_01/images/drawing}
\includegraphics[width=7cm]{python_codes/gravity_01/images/drawing}
\end{center}

Assume that this domain is filled with a rock type which
Expand Down Expand Up @@ -65,7 +65,7 @@
measured at each gravimeter at the surface.

\begin{center}
\includegraphics[width=12cm]{/home/cedrict/Desktop/FIELDSTONE/fieldstone/python_codes/gravity_01/solution.pdf}
\includegraphics[width=12cm]{python_codes/gravity_01/solution.pdf}
\end{center}


Expand Down