Wireline Standard Data Processing
ODP logging contractor: LDEO-BRG
Hole: 1170D
Leg: 189
Location: South Tasman Rise (Tasman
Sea)
Latitude: 47° 9.04'S
Longitude: 146° 2.991'E
Logging date: April, 2000
Bottom felt: 2715.8 mbrf
Total penetration: 779.8 mbsf
Total core recovered: 287.69 m (81.1
%)
Logging
Runs
Logging string 1: DIT/APS/HLDS/HNGS (2
passes)
Logging string 2: GHMT/DSI/NGT (2 passes)
Logging string 3: FMS/DSI/NGT (4 passes)
The plan at this hole was to log in two
stages: first the lower part, with the pipe set at about 533 mbsf (below
anticipated bridges), and then the upper part after raising the pipe. Good
logging data was obtained for the lower 250 m of the hole; the anticipated
logging of the upper part of the hole, however, was not possible, because after
logging the lower part, the pipe was found to be stuck and had to be exploded
off just above the BHA. The DSI did not record logs during passes 2, 3 and 4 of
the FMS/DSI/NGT tool string.
Bottom-hole
Assembly
The following bottom-hole assembly depths are
as they appear on the logs after depth matching (see "Depth shift"
section) and depth shift to the sea floor. As such, there might be a
discrepancy with the original depths given by the drillers onboard. Possible
reasons for depth discrepancies are ship heave, drill string and/or wireline
stretch, and tides.
DIT/APS/HLDS/HNGS: Bottom-hole assembly at
533 mbsf (pass 1)
GHMT/DSI/NGT: Bottom-hole assembly at 533
mbsf (passes 1 and 2)
FMS/DSI/NGT: Bottom-hole assembly at 533.5
(pass 4)
Processing
Depth shift: Since the depth match between the total gamma of the
DIT/APS/HLDS/HNGS and GHMT/DSI/NGT logging runs is somewhat ambiguous, the
conductivity from the GHMT (MAGC) was matched to the DIT from the
DIT/APS/HLDS/HNGS second pass. Then the SGR gamma ray logs from the FMS/DSI/NGT
tool string were matched to the shifted SGR log from the GHMT/DSI/NGT tool
string (pass 1) because the FMS/DSI/NGT lacked a resistivity or conductivity
log. Finally, all the logs were shifted to the sea floor (-2711.8 m). The
mudline was not logged; according to the logs, however, the end of the bottom
hole assembly was 4 m shallower than according to the drillers. Therefore the
logger's sea-floor is also taken to be 4 m shallower.
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 then the
features in the equivalent logs from the other runs are matched to it in turn.
This matching is performed automatically, and the result checked and adjusted
as necessary. 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 wireline heave compensator stopped at
certain intervals during logging, because of excessive ship heave. Depth
control is degraded in these intervals, and consequently the match between
different runs, and even between different tools on the same tool string will
be poor. These intervals are: 662-693 and 736-763 mbsf (DIT/APS/HLDS/HNGS pass
1), 631-672 mbsf (DIT/APS/HLDS/HNGS), 712-747 mbsf (GHMT/DSI/NGT pass 1),
584-610 mbsf (GHMT/DSI/NGT pass 2).
Gamma-ray processing: The gamma ray logs from the NGT have been
re-processed to account for borehole size and drilling fluid. The HNGS data
were corrected for hole size during logging.
Acoustic data processing: The DSI waveform data were processed during logging to
give DTCO (compressional wave slowness) and DTSM (shear wave slowness). DTCO
and DTSM from the main pass (pass 4) are good and match well to the repeat
passes (GHMT/DSI/NGT pass 2 and FMS/DSI/NGT pass 1). The DTSM appears to have
unreasonable values from 268-273 mbsf. From 300-538 mbsf there is high
amplitude DTCO variability that has no corresponding variability in the DTCO,
thus the shear velocity data in this interval should be regarded with caution.
No editing was performed, and the compressional and shear slownesses were then
converted to velocities.
High-resolution data: Bulk density and neutron porosity data were recorded
at a sampling rate of 2.54 and 5.08 cm respectively. The enhanced bulk density
curve is the result of Schlumberger enhanced processing technique performed on
the MAXIS system onboard. While in normal processing short-spacing data is
smoothed to match the long-spacing one, in enhanced processing this is
reversed. In a situation where there is good contact between the HLDS pad and
the borehole wall (low density correction) the results are improved, because
the short-spacing has better vertical resolution.
Quality
Control
Null value=-999.25. This value may replace
invalid log values or results.
Large (>12") and/or irregular
borehole affects most recordings, particularly those that require
eccentralization (APS, HLDS) and a good contact with the borehole wall. The
logged portion of Hole 1170D was smooth, with a hole diameter between 10-11
inches, with only one washout at 647-649 mbsf. Consequently, the log quality is
generally excellent.
Data recorded through bottom-hole assembly,
such as the gamma ray data, should be used qualitatively only because of the
attenuation on the incoming signal.
Hole diameter was recorded by the hydraulic
caliper on the HLDS tool (LCAL) and by the caliper on the FMS tool string.
Additional information about the logs can be
found in the "Explanatory Notes" and Site Chapter, ODP IR volume 189.
For further questions about the logs, please contact:
Cristina Broglia
Phone: 845-365-8343
Fax: 845-365-3182
E-mail: Cristina Broglia