Standard Wireline Data Processing
Science operator: Texas A&M University
Hole: U1470B
Expedition: 359
Location: Maldive Archipelago (central equatorial N Indian Ocean)
Latitude: 4° 45.9818' N
Longitude: 72° 59.0210' E
Logging date: November 17, 2015
Sea floor depth (driller's): 410.8 m DRF
Sea floor depth (logger's): 405.5 m WRF
Total penetration: 754.5 m DRF (343.7 m DSF)
Total core recovered: 147.13 m (40.3 % of cored section)
Oldest sediment recovered:
Lithology: Sands at the top, coral and limestone at the bottom.
The logging data
was recorded by Schlumberger in DLIS format. Data were processed at the
Borehole Research Group of the Lamont-Doherty Earth Observatory in November 2015.
Tool string | Pass
|
Top depth (m WMSF) | Bottom depth (m WMSF) | Pipe depth (m WMSF) | Notes |
1.HRLA/DSI/HLDS/EDTC-B/HNGS
|
Downlog
|
103.5 |
Caliper closed and no HLDS source. No density data.
|
||
Uplog
|
103.5 |
Caliper closed and no HLDS source. No density data.
|
Logging at Hole U1470B was carried out on short notice; while hole conditions were known to be far from ideal, scientists were hoping to get some wireline data. Therefore, it was decided to run a modified tool string combination, which included resistivity, sonic, density and gamma ray tools (HRLA/DSI/HLDSEDTC-B/HNGS). The HLDS was included in order to get a caliper emasurement, but no nuclear source was mounted. The total drilling depth of 754.5 m DRF was never reached; there was a significant loss of tension at 520 m WRF, about 10 m outside the drill pipe. After several attempts to go deeper the string finally reached 463 m WRF but it would not go any further. Data were acquired uplog from that depth and logging operations were terminated.
The sea state was calm, therefore no Wireline Heave Compensator (WHC) was used.
The depths in
the table are for the processed logs (after depth shift to the sea floor and depth matching between passes). 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 a 'bottom felt' depth in soft sediment.
Depth shift to sea floor and depth match.
The original logs were first shifted to the sea floor (-
405.5 m). The sea floor depth
was determined by the step in gamma ray values observed on the HRLA/DSI/HLDS/HNGS downlog at 405.5 m WRF. This differs by 5.3 m from the sea floor depth given by the drillers (see
above). The depth-shifted logs have then been depth-matched to the gamma ray log from the downlog of the HRLA/DSI/HLDS/HNGS tool string. Though the downlog was shorter than the uplog, it was chosen as the reference run because the sea floor was more clearly identified than on the uplog.
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.
Environmental corrections. The HNGS and HRLA data were corrected for hole size during the recording.
High-resolution data. Gamma Ray data from the EDTC-B tool were recorded at sampling rates of 5.08 and 15.24 cm.
Acoustic data. The dipole shear sonic imager (DSI) was operated in the following modes: P&S monopole, upper dipole, and Stonely mode in standard frequency, and lower dipole mode in lower frequency. However, the open hole logged interval was too short to acquire any acoustic data.
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 of the incoming signal. The
thick-walled BHA attenuates the signal more than the thinner-walled drill pipe.
The caliper tool on the HLDS tool, which measures the hole diameter, was kept closed during the entire logging operations in order to minimize the risk of losing the tool string in the rapidly deteriorating hole.
A null value of
-999.25 may replace invalid log values.
Additional information about the drilling and logging operations can be found in the Operations and Downhole Measurements sections of the expedition report, Proceedings of the International Ocean Discovery Program, Expedition 359. For further questions about the logs, if the hole is still under moratorium please contact the staff scientist of the expedition.
After the moratorium period you may direct your questions to:
Cristina Broglia
Phone: 845-365-8343
Fax: 845-365-3182
E-mail: Cristina Broglia
Tanzhuo Liu
Phone: 845-365-8630
Fax: 845-365-3182
E-mail: Tanzhuo Liu