commit 95b4a750ffa7a77d405dcca11cb9a5a9128efac7
parent d6896552d938a8670a831612069f06624d2c1dad
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Wed, 18 Dec 2019 17:00:11 +0100
Fix reference to van der Meer 2009
Diffstat:
1 file changed, 1 insertion(+), 1 deletion(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -342,7 +342,7 @@ Albeit at shallower depths, deformation is still expected to occasionally occur
Other water-pressure forcings may be additional mechanisms for deep deformation if they cause minima in effective stress at depth.
For example, lateral water input from lake drainage or hydrological rerouting may also create episodes of deep slip, in particular when horizontal bedding decreases vertical permeability \cite<e.g.,>[] {Kjaer2006}.
-Water-escape structures are commonly observed in till deposits \cite<e.g.,> {vanDerMeer2009, Knight2015, Salamon2016, Ingolfsson2016}, which indicates that overpressurization of water within till beds may be extremely common.
+Water-escape structures are commonly observed in till deposits \cite<e.g.,> {van_der_Meer2009, Knight2015, Salamon2016, Ingolfsson2016}, which indicates that overpressurization of water within till beds may be extremely common.
Since tills fail at their weakest spot, we suggest that subglacial deformation may not only be a patchy mosaic of deforming spots in the horizontal plane \cite<e.g.,> {Piotrowski2004}, but also at depth.