GVR Image Processing Report


The LWD (Logging While Drilling) GVR tool maps the electrical resistivity of the borehole wall at three depths of penetration. Because the tool is rotating while drilling, its three electrodes (one for each penetration depth) provide 360° data coverage of the borehole wall. These data are displayed as an electrical image of the formation in either gray or color scale. The purpose of this report is to describe the images from the Chevron Gulf Mexico Gas Hydrate JIP Drilling Program and the different steps used to generate them from the raw GVR measurements. The GVR tool also takes total gamma radiation and resistivity logs, which are presented with the standard data.

IODP drilling and logging operator: CDEX

Hole: C0002F

Expedition: 338

Location: Nankai Trough (NW Pacific Ocean)

Latitude: 33° 18.0507' N

Longitude: 136° 38.2029' E

Logging-while-drilling date: November 2-13, 2012

Sea floor depth: 1967.5 m LRF

Total penetration: 3973 m LRF (2005.5 m LSF)

Image interval: 874-2006 mbsf

Azimuth Reference (P1AZ): -6.74°


Data Quality


Horizontal artifacts due to the ship's heave are observed throughout the logged interval. There are also intervals of missing data due to high stick-slip. Drilling cork-screw artifacts can be observed at the following depths: 892-907, 923-932, 1087-1097, 1241-1250, and 1485-1492,m LSF.

The rate of penetration was approximately 35 m/hr until about 1006 m LSF; below this depth it dropped to about 12 m/hr.


Image Processing


Processing is required to convert the electrical current in the formation, emitted by the GVR button electrodes, into a gray or color-scale image representative of the resistivity changes. This is achieved through two main processing phases, the first shortly after the data is downloaded from the tool by the Schlumberger engineer, and the second post-cruise at LDEO-BRG.


1) Azimuthal orientation and conversion to depth


The main processing steps are performed using Schlumberger's Ideal software package by the Schlumberger LWD engineer, just after the raw data is downloaded from the tool. An azimuth and a depth are assigned to each measurement based on measurements of the pipe orientation and position at the rig floor. The resistivity measurements are assigned to 56 radial bins (each 6.4° wide). A full 360° revolution of resistivity data is sampled every 10 (or 20) seconds, therefore the data density in terms of depth depends upon the rate of penetration (ROP) into the formation – the slower the penetration, the more densely sampled the formation will be. For this hole, the ROP was in the 15-35 m/hr range.


The GVR tool does not move with a constant velocity down the hole: new sections of drill pipe have to be added every 10 m and ship heave is never completely compensated. This means that there will often be repeat measurements for one particular depth in the borehole. The measurement that is used is the first one taken at a particular point, before the borehole has had time to deteriorate.


The effects of ship heave are sometimes apparent as horizontal discontinuities in the image. They exist because it can be difficult, with a long drill string, to accurately determine the depth of the bit based on measurements on the rig floor.


The GVR data is output from the Ideal software as a depth-indexed DLIS file.


2) Image Normalization:


The DLIS file is loaded into the Schlumberger GeoQuest GeoFrame software at LDEO-BRG, where the depth-based image for each depth of penetration (shallow, medium, and deep) is normalized both statically and dynamically.


In 'static normalization', a histogram equalization technique is used to obtain the maximum quality image. In this technique, the resistivity range of the entire interval of good data is computed and partitioned into 256 color levels. This type of normalization is best suited for large-scale resistivity variations.


The image can be enhanced when it is desirable to highlight features in sections of the well where resistivity events are relatively subdued when compared with the overall resistivity range in the section. This enhancement is called 'dynamic normalization'. By rescaling the color intensity over a smaller interval, the contrast between adjacent resistivity levels is enhanced. It is important to note that with dynamic normalization, resistivities in two distant sections of the hole cannot be directly compared with each other. A 6-ft normalization interval is used.


The normalized images are shifted to a sea-floor reference and converted to gif files using in-house software. They are presented in the downhole log online database. The image is displayed as an unwrapped borehole cylinder. A dipping plane in the borehole will be displayed as a sinusoid on the image; the amplitude of this sinusoid is proportional to the dip of the plane. The images are oriented with respect to the north, hence the strike of dipping features can also be determined.


Additional information about the drilling and logging operations can be found in the Operations and Downhole Measurements sections of the expedition reports, Proceedings of the Integrated Drilling Program, Expedition 338. For further questions about the online database please contact:


Phone: 845-365-8343

Fax: 845-365-3182

E-mail: Cristina Broglia


For questions about the processing of the resistivity images please contract:


Tanzhuo Liu

Phone: 845-365-8630

Fax: 845-365-3182

E-mail: Tanzhuo Liu


For questions about the logs, please contact:


Yoshinori Sanada

E-mail: sanada@jamstec.go.jp


Yukari Kido

Email: ykido@jamstec.go.jp


Yuichi Shinmoto