From 1b6822bb2aa864a190cd8351e804d60e9e327bb6 Mon Sep 17 00:00:00 2001
From: Elias Pipping <elias.pipping@fu-berlin.de>
Date: Tue, 30 Oct 2012 14:48:39 +0100
Subject: [PATCH] Kill some comments

---
 src/one-body-sample.parset | 20 --------------------
 1 file changed, 20 deletions(-)

diff --git a/src/one-body-sample.parset b/src/one-body-sample.parset
index 78861e1f..b5c30ef1 100644
--- a/src/one-body-sample.parset
+++ b/src/one-body-sample.parset
@@ -55,23 +55,3 @@ V0 = 1
 L = 1e-5
 initial_log_state = -10
 state_model = Dieterich
-
-# The second-order a and b terms in [..] are very important in
-# determining whether sliding is stable or unstable and (in appli-
-# cation to the Earth) whether an earthquake or stable creep
-# occurs. From [..], velocity strengthening and thus stable creep
-# occurs when a is greater than b.  If b > a, instability can occur
-# unless the "spring" supplying stress to the fault or sample is too
-# stiff
-# -- Norman H.  Sleep:
-# Application of a unified rate and state friction theory to the
-# mechanics of fault zones with strain localization
-
-# If a > b, the overall change of f is positive, the friction is
-# velocity-strengthening, and only stable sliding is possible. On the
-# other hand, if a < b, the overall change is negative, the friction
-# is velocity-weakening, and dynamic instabilities can occur (e.g.,
-# Ruina, 1983). The situation a < b provides a necessary but not a
-# sufficient condition for instability.
-# -- Yehuda Ben-Zion:
-# Dynamic ruptures in recent models of earthquake faults
-- 
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