Wireline Standard Data Processing
DSDP operator and logging contractor: Scripps Institution of Oceanography
Hole: 568
Leg: 84
Location: Mid America Trench Slope (tropical NE Pacific)
Latitude: 13° 4.33' N
Longitude: 90° 48.00' W
Logging date: February 1982
Sea floor depth (drillers' mudline): 2031 mbrf
Sea floor depth (step in GR log): 2036.5 mbrf
Total penetration: 417.7 mbsf
Total core recovered: 308.4 (73.8 % of cored section)
Oldest sediment cored: early Miocene
Lithologies: biogenic mud with ash layers, sandy mud. Gas hydrates present.
The logging data was recorded by Schlumberger in LIS format. Data were processed at the Borehole Research Group at the Lamont-Doherty Earth Observatory in December 2003.
| Tool string | Pass | Top depth (mbsf) | Bottom depth (mbsf) | Bit depth (mbsf) | Notes |
| 1. LSS/GR |
lower
|
234
|
408
|
|
SWF recorded
|
|
upper
|
76
|
235
|
|
SWF recorded
|
|
|
main
|
|
77
|
405
|
|
|
| 2. FDC/CNL/GR |
main
|
0
|
408
|
reference
|
|
| 3. FDC/LSS/GR |
repeat
1
|
78
|
207
|
|
|
|
repeat
2
|
174
|
194
|
|
|
The logging tool strings were able to reach the bottom of the hole without problem. The DIT induction tool was run on the FDC/LSS/GR tool string, but did not record data. The CNL porosity tool on the FDC/CNL/GR tool string did not record data. The LSS on FDC/LSS/GR repeat 1 did not record data. The DSDP volume says there were two tool strings, but the names of the tools in the data files indicate there were three tool strings (see table above).
The depths in the table are for the processed logs (after depth matching between passes and depth shift to the sea floor). Generally, discrepancies may exist between the sea floor depths determined from the downhole logs and those determined by the drillers from the pipe length. Typical reasons for depth discrepancies are ship heave, wireline and pipe stretch, tides, and the difficulty of getting an accurate sea floor from the 'bottom felt' depth in soft sediment.
Depth match and depth shift to sea floor: The original logs were depth-matched to the GR log from the main pass of the FDC/CNL/GR tool string, and were then shifted to the sea floor (- 2036.5 m). The FDC/CNL/GR main pass was chosen as the reference run because it was the only run to cross the sea floor. The GR logs from the other passes were matched to the GR log from the reference run.
Depth-matching is typically done in the following way. One log is chosen as reference (base) log (usually the total gamma ray log from the run with the greatest vertical extent and no sudden changes in cable speed), and then the features in the equivalent logs from the other runs are matched to it in turn. This matching is performed manually. The depth adjustments that were required to bring the match log in line with the base log are then applied to all the other logs from the same tool string.
The sea floor depth was determined by the step in gamma ray values at 2036.5 mbrf. This differs by 5.5 m from the sea floor depth given by the drillers (see above). With this hole, there is also a minor step in gamma ray values at 2033 mbrf, but it was not used because it is smaller than the step at 2036.5 mbrf.
Sonic data: The transit time data were processed using an in-house program that compares the slowness derived from the 8 different transmitter-receiver combinations at each depth, and discards those times that are significantly different from the majority as bad data. The 'points' column in the LSS data files is a measure of confidence: it records the number of transmitter-receiver pairs retained - a value of 8 means that no data was discarded. This processing leads to improved compressional wave velocity logs that are free of the artifacts present in the velocities derived directly from DT and DTL. For Hole 568, the Main, Lower, and Upper LSS data was processed in this way, but the repeat passes did not record the four travel times and so we had to calculate the velocity directly from the slowness, DT.
The quality of the data is assessed by checking against reasonable values for the logged lithologies, by repeatability between different passes of the same tool, and by correspondence between logs affected by the same formation property (e.g. the resistivity log should show similar features to the sonic velocity log).
Gamma ray logs recorded through bottom hole assembly (BHA) and drill pipe should be used only qualitatively, because of the attenuation on the incoming signal. The thick-walled BHA attenuates the signal more than the thinner-walled drill pipe. (The CNL porosity can sometimes be used qualitatively through the BHA and pipe, but most of the other logs will not give usable data.)
A wide (>12") and/or irregular borehole affects most recordings, particularly those that require eccentralization and a good contact with the borehole wall (FDC, CNL). Hole diameter was recorded by the hydraulic caliper on the FDC tool (CALI) and by the 3-arm MCD tool (CALI). The caliper on the FDC tool appears to be the more reliable of the two devices, giving hole diameters varying from 9-13 inches.
A null value of -999.25 may replace invalid log values.
Additional information about the drilling and logging operation can be found in the Operations section of the Site Chapter in DSDP Initial Reports volume 84. For further questions about the logs, please contact:
Cristina Broglia
Phone: 845-365-8343
Fax: 845-365-3182
E-mail: Cristina Broglia