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Start: July 1996 (month 5)
End: December 1997 (month 22)
Responsible partner: GFZ.DR.DBL
As described in the previous reports, three logging campaigns took place in
1996. During these campaigns, repeated measurements were performed in well
LL-03 (Nefsholt). In cooperation with Orkustofnun, logging was done in 5 other
boreholes, of which at least the borehole-televiewer measurements in well
LJ-08 are relevant for this project.
The recent activities within this subproject comprise two logging campaigns in
1997, one in September, the second in December. The first was exclusively
concerned with repeated logging in borehole LL-03 (Nefsholt) inside the SISZ.
During the second campaign, additional logs were run with the
borehole-televiewer in Bödmódsstadir (located at the northern edge of the SISZ,
close to Laugarvatn) and in Thykkvibær (slightly south of the SISZ, near the
south coast). The latter borehole was drilled very recently. The locations are
shown in Figure 22.
Figure 22:
Map of the south-western part of Iceland showing the
location of the site of repeated logging (Nefsholt) and
of the other two boreholes where borehole-televiewer
measurements have been performed during 1997.
|
Table 1 shows the logs performed during the first
and second year of this project.
These five campaigns have thus attributed to the two aims of this subproject:
-
- Observation of changes in physical parameters of the rock and
of changes in degree of fracturing and orientation of
principal stresses with respect to seismic activity.
-
- Indirect measurement of tectonic stress orientation to
evaluate the tectonic stress field in the area of the SISZ.
Table:
As borehole NG-01 partly collapsed between log
runs, the hole was abandoned and well LL-03 was chosen for repeated logging.
GR indicates Gamma-Ray-log, SP stands for Spontaneous Potential.
FED means Four-Arm-Dipmeter which includes an oriented four-arm-caliper.
BHTV means ultrasonic Borehole-Televiewer.
BCS is Borehole-Compensated-Sonic; DIL is Dual-Induction/Latero log.
For technical reasons, no FED run was possible in LL-03,
no BHTV run was possible in LJ-08 below 1330 m depth,
no BHTV run was possible in BS-11 above 703 m depth.
Due to the limited availability of a crane, no BHTV or FED run were possible
in TN-02.
The deepest parts of wells LJ-08, LL-03, THB-13 and BS-11 were not
accessible anymore.
Name: |
Location: |
Max. |
Logged |
Tools used: |
Date: |
|
|
depth: |
interval: |
|
|
NG-01 |
Ólafsvellir |
1070 m |
180-1070 m |
FED, GR, SP, |
July 1996 |
|
(inside SISZ) |
|
|
3-arm-caliper, |
|
|
|
|
|
16"- and 64"- |
|
|
|
|
|
resistivity |
|
HS-36 |
Reykjavík |
980 m |
330-980 m |
BHTV, BCS-GR |
July 1996 |
LPN-10 |
Laugaland |
890 m |
80-880 m |
BHTV, |
July 1996 |
|
near Akureyri, |
|
|
BCS-DIL-GR |
|
|
North Iceland |
|
|
|
|
LJ-08 |
Sydra Laugaland |
2740 m |
120-1890 m |
FED, BHTV, |
July 1996 |
|
near Akureyri |
|
120-1330 m |
BCS-DIL-GR |
|
TN-02 |
Ytri-Tjarnir |
1370 m |
260-1370 m |
BCS, GR |
July 1996 |
|
near Akureyri |
|
|
|
|
LL-03 |
Nefsholt |
1309 m |
80-1100 m |
BHTV, BCS-DIL-GR, |
July 1996 |
|
(inside SISZ, |
|
|
neutron-neutron, |
October 1996 |
|
site of repeated |
|
|
X-Y-caliper, |
September 1997 |
|
logging) |
|
|
16"- and 64"- |
December 1997 |
|
|
|
|
resistivity, SP |
|
THB-13 |
Thykkvibær |
1254 m |
466-1225 m |
BHTV |
December 1997 |
|
south-west of Hella |
|
|
|
|
|
near the south coast |
|
|
|
|
BS-11 |
Bödmódsstadir |
1193 m |
703-1090 m |
BHTV |
December 1997 |
|
near Laugarvatn |
|
|
|
|
|
Next: Task 2: Check for
Up: Subpart 4A: Geophysical loggings
Previous: Subpart 4A: Geophysical loggings
Gunnar Gudmundsson
1999-03-17