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Task 1: Logging activities

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.
\includegraphics[width=\textwidth]{/heim/gg/pren1/final/roth/4A-1.eps}

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:

$\bullet$
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.
$\bullet$
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 up previous contents
Next: Task 2: Check for Up: Subpart 4A: Geophysical loggings Previous: Subpart 4A: Geophysical loggings
Gunnar Gudmundsson
1999-03-17