Standard Wireline Data Processing

 

 

Science operator: Texas A&M University

Hole: U1464C

Expedition: 356

Location: Roebuck Basin (Tropical SE Indian Ocean)

Latitude: 18° 3.9244' S

Longitude: 118° 37.8942' E

Logging date: September 23, 2015

Sea floor depth (driller's): 275.3 m DRF

Sea floor depth (logger's): 276 m WRF (MSS/HRLA/APS/HLDS/EDTC/HNGS downlog)

Total penetration:  1115.3 m DRF (840 m DSF)

Total core recovered: 94.03 m (17.7 % of cored section)

Oldest sediment recovered: Middle Miocene

Lithology: Dolomitic grainstone, packstone, wackestone, mudstone.

 

 

Data

 

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 September 2015.

 

Logging Runs

 

Tool string
Run/Pass
Top depth (m WMSF)
Bottom depth (m WMSF)
Pipe depth (m WMSF)
Notes
1. MSS/HRLA/APS/HLDS/EDTC/HNGS
Downlog
0
783
84
Closed caliper. Invalid HLDS and APS.
Main
615
783
recorded open hole

 

Hole U1464C was drilled with 9 7/8" bit down to 840 m DRF (564.7 m DSF). The drill pipe was placed at ~86.7 m DSF to guide the logging tools into the open hole. The MSS/HRLA/APS/HLDS/EDTC/HNGS tool string acquired a downlog and a short uplog. The uplog was intended to be a repeat section until the string stopped due to excessive tension. After closing the caliper tool it was inferred that a hole collapse might have occurred above the tool. Recovery of the tool string and of its nuclear sources became the primary objective of the logging operation, which concluded succesfully with an undamaged tool after lowering enough pipe to clear any bridge.

 

The wireline heave compensator (WHC) was utilized on both MSS/HRLA/APS/HLDS/EDTC/HNGS passes. The ship's peak-to-peak heave averaged 0.6 m.

 

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.

 

Processing

 

Depth shift to sea floor and depth match. The original logs were first shifted to the sea floor (-276 m). The sea floor depth was determined by the step in gamma ray values obcserved on the MSS/HRLA/APS/HLDS/EDTC/HNGS downlog at 276 m WRF. This differs by 0.7 m from the sea floor depth of 275.3 m DRF given by the drillers. The depth-shifted logs have then been depth-matched to the gamma ray log from the downlog of the MSS/HRLA/APS/HLDS/EDTC/HNGS tool string.

 

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. The APS and HLDS data were corrected for standoff and hole size respectively during the recording.

 

Quality Control

 

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. The overall quality of the data from Hole 1464C is good.

 

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.

 

Hole diameter was recorded by the hydraulic caliper on the HLDS tool (LCAL). The HLDS caliper indicatea a large hole (> 16"), which becomes increasingly rugged above 520 m WMSF as the tool string approaches the depth where it became stuck. No caliper data were acquired in the upper part of the hole after the recovery operation started.

 

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 356. 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