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An experimental investigation of dyke injection under
regional extensional stress
Katherine A. Daniels, Thierry Menand
To cite this version:
∆
∞
z
z = x + iy
Z
s
s
σ
s
σ
γ
-
σ
y/P
Iσ σ
σ
ε
xε
yx
y
σ σ
σ
x y
z
σ
σ
σ
UN
Silsa Extension directionD
30o -30o 0o 0o 30oA
Red Sea Gulf of Aden Somalia Yemen Afar Eritrea Sudan Addis Ababa ETHIOPIAMain Ethiopian Rift
Djibouti
B
Recent Dykes Dabbahu Gabho Ado ‘Ale Volcanic Complex Semara 0 500 1000 1500 2000 Elevation (m) SilsaN
C
20 10 0 10 20 30 40 50 60 70 1981 1980 1979 1978 1977 1982 1983 1984 1976 1975 2013 2012 2011 2010 2009 2008 2007 2006 80 2005 1 2 3 4Afar rifting episode 2005-2009
Krafla rifting episode 1975-1984
Distance along rift segment (km)
Year
E
B C
Gelatine block
Layer 2 = 10 L
Layer 1 = 29 L
Injections
TANK 1
Injections
TANK 1
C)
A)
Gelatine block
Layer 2 = 10 L
TANK 1
Layer 1 = 29 L
Injections
Metal heating plate
A)
B)
C)
D)
Plan-view
Plan-view
Side-view
Side-view
Injection 1
Injection 1
20 cm
20 cm
20 cm
20 cm
Propagation direction of
later dyke changes once
tip of later dyke has past
the end of the first dyke.
0
1
2
3
4
5
6
7
8
9
10
0
10
20
30
40
50
60
70
80
Injection Spacing (cm)
Rotation Angle (degrees)
Extension = 0.01 m
Extension = 0.02 m
Extension = 0.03 m
First Injections
-1 -1 -0. 8 -0.8 -0.6-0.4 -0.6 -0.4 -0.2 -0.2 -0.2 -0.2 0 0 0 0 0 0 0. 2 0.2 0.2 0.2 0. 4 0.4 0.4 0.6 0.6 0.8 0.8
1
2
3
0
-3
-2
-1
1
2
3
Dir
ec
tion nor
mal t
o the dyke (y)
x
y
y
x
Displacement of the solid
Maximum aperture
A)
B)
spatial evolution of the normal stress
spatial evolution of the approxi-mation of the normal stress
residual