IODP operator and logging contractor: LDEO-BRG
Hole: 642E (ODP re-entry hole)
Expedition: 306
Location: Voring Plateau (Norwegian Sea)
Latitude: 67° 13.2' N
Longitude: 2° 55.8' E
Logging date: July 1985
Logging date: October 1983
Sea floor depth (driller's): 1289 mbrf
Total penetration: 1229.4 mbsf
Total core recovered: 372.6 m (41.1 % of cored section)
Oldest sediment cored: Fine-grained volcaniclastic sediment (Early Eocene)
Lithologies: Glacial muds, nannofossil and siliceous oozes, volcaniclastic muds, sandy muds, and sand (sediments); tholeitic basalt flows and basaltic-andesite flows (basement)
FMS Pass 1: 372-592 mbsf
FMS Pass 2: 372-443 mbsf
Magnetic
declination: -4.01°
Water depth: 1289 mbrf
The basic
principle of the FMS (Formation MicroScanner) is to map the conductivity of the
borehole wall with a dense array of sensors. This provides a high resolution
electrical image of the formation which can be displayed in either gray or
color scale. The purpose of this report is to describe the images from
Expedition 305 and the different steps used to generate them from the raw FMS
measurements.
The FMS tool
records 4 perpendicular electrical images, using four pads, which are pressed
against the borehole wall. Each pad has 16 buttons and the tool provides
approximately 25% coverage of the borehole wall. The tool string also contains
a triaxial accelerometer and three flux-gate magnetometers (in the GPIT,
General Purpose Inclinometry Tool) whose results are used to accurately orient
and position the images. Measurements of hole size, cable speed, and natural
gamma ray intensity also contribute to the processing.
Data Quality
Excellent borehole images were obtained from Hole 642E. The hole is generally in gauge (10 inches wide), but with some 1-5 m-thick intervals extending to 16 inches or wider.
The lithology of the logged interval includes basalt flows and basalt breccias.
Processing is
required to convert the electrical current in the formation, emitted by the FMS
button electrodes, into a gray or color-scale image representative of the
conductivity changes. This is achieved through two main processing phases: data
restoration and image display.
1) Data
Restoration
Speed
Correction. The data from the z-axis accelerometer is used to correct the
vertical position of the data for variations in the speed of the tool ('GPIT
speed correction'), including 'stick and slip'. In addition, 'image-based speed
correction' is also applied to the data: the principle behind this is that if
the GPIT speed correction is successful, the readings from the two rows of
buttons on the pads will line up, and if not, they will be offset from each
other (a zigzag effect on the image).
Equalization:
Equalization is the process whereby the average response of all the buttons of
the tool are rendered approximately the same over large intervals, to correct
for various tool and borehole effects which affect individual buttons
differently. These effects include differences in the gain and offset of the
pre-amplification circuits associated with each button, and differences in
contact with the borehole wall between buttons on a pad, and between pads.
Button
Correction. If the measurements from a button are unreasonably different from
its neighbors (e.g. 'dead buttons') over a particular interval, they are
declared faulty, and the defective trace is replaced by traces from adjacent
good buttons.
EMEX voltage
correction. The button response (current) is controlled by the EMEX voltage,
which is applied between the button electrode and the return electrode. The
EMEX voltage is regulated to keep the current response within the operating
range. The button response is divided by the EMEX voltage so that the response
corresponds more closely to the conductivity of the formation.
Depth-shifting: Each of the logging runs are 'depth-matched' to a common scale by means of lining up distinctive features of the natural gamma log from each of the tool strings. If the reference logging run is not the FMS tool string, the specified depth shifts are applied to the FMS images. The position of data located between picks is computed by linear interpolation.
2) Image
Display: Once the data is processed, both 'static' and 'dynamic' images are
generated; the differences between these two types of image are explained
below. Both types are provided online and on CD-ROM.
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 2-m normalization
interval is used.
Interested
scientists are welcome to visit the log interpretation centers at LDEO if they wish to use the image generation and interpretation software.
Oriented
Presentation: The image is displayed as an unwrapped borehole cylinder (its
circumference is derived from the bit size). Several passes can be oriented and
merged together on the same presentation to give additional borehole coverage
if the tool pads followed a different track. 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
north, hence the strike of dipping features can also be determined.
For further information or questions about the processing,
please contact:
Cristina Broglia
Phone: 845-365-8343
Fax: 845-365-3182
E-mail: Cristina Broglia