[cig-commits] commit: Added more detail to the large strain information.
Mercurial
hg at geodynamics.org
Sun Feb 10 21:33:05 PST 2013
changeset: 173:e4a3ef813c7a
tag: tip
user: Charles Williams <C.Williams at gns.cri.nz>
date: Mon Feb 11 18:32:53 2013 +1300
files: faultRup.tex
description:
Added more detail to the large strain information.
diff -r 1b19a2d00c03 -r e4a3ef813c7a faultRup.tex
--- a/faultRup.tex Mon Feb 11 17:24:26 2013 +1300
+++ b/faultRup.tex Mon Feb 11 18:32:53 2013 +1300
@@ -515,9 +515,11 @@ This matches the tangent stiffness matri
This matches the tangent stiffness matrix in conventional solid
mechanics finite-element formulations. In computing the residual, we
use the expression given in equation~(\ref{eqn:residual:elasticity})
-with one implementation for infinitesimal strain and another implementation
-for small strain and rigid body motion. Following a similar procedure,
-we find the portion of the Jacobian associated with the constraints,
+with one implementation for infinitesimal strain and another
+implementation, employing the Green-Lagrange strain tensor and the
+second Piola-Kirchoff stress tensor, for small strain with moderate
+amounts of rigid body motion. Following a similar procedure, we find
+the portion of the Jacobian associated with the constraints,
equation~(\ref{eqn:quasi-static:residual:fault}), is
\begin{linenomath*}\begin{equation}\label{eqn:jacobian:constraint}
\bm{L} = \int_{S_f} \bm{N}_p^T \cdot (\bm{N}_{n^+} - \bm{N}_{n^-}) \, dS.
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