geothermal resource potential of the safford-san simon basin, arizona

LINE 7 RESISTIVITY
N =2000 FEET, DIPOLE-DIPOLE ELECTRODE CONFIGURATION
N lOW 8W 6W 4W 2W 0 2E 4E 6E 8E IOE 12E
I
PSEUDOSECTION
2
OF
3
APPARENT
4
RESISTIVITY
Ohm-meters
5l..-.__--::~---.b,...._-~......,I:_____r--_!o_--__:~---_+_---l
N lOW 8W 6W 4W
I
2
3
4
5
PSEUDOSECTION
OF MODEL
APPARENT
RESISTIVITY
Ohm - meters
~ 0
~ 10,00
~ 2000
~
j}
3000
'1 4000
10
20
30
o
I------t
2000 Feet
RESISTIVITY
SUBSURFACE
MODEL
Ohm - meters
LINE 8 RESISTIVITY
N lOW
8W
N= 2000 FEET, DIPOLE-DIPOLE ELECTRODE CONFIGURATION
6W 4W2W 0 2E 4E 6E 8E 10E 12E
I
2
3
4
5
N lOW
I
2
3
4
5
8W
PSEUDOSECTION
OF
APPARENT
RESISTIVITY
Ohm-meters
PSEUDOSECTION
OF MODEL
APPARENT
RESISTIVITY
Ohm - meters
...... 0
~ 1000
~ 2000
~ 3000
~
~ 4000
"""301
20 20
I
10 r5
I
50 30
I I 3 I L!-
I
10
5 I
1
I 0.4
0 2000 FEET I I 5
I---j
RESISTIVITY
SUBSURFACE
MODEL
Ohm-meters
Figure 19.
Subsurface resistivity models and pseudosections
of resistivity profiles 7 and 8.
55