FMS Image Data Processing
ODP logging
contractor: LDEO-BRG
Hole: 995B
Leg: 164
Location: Blake Ridge (NW Atlantic Ocean)
Latitude: 31° 48.244' N
Longitude: 75° 31.360' W
Logging date: November, 1995
Bottom felt: 2785 mbrf
Total penetration: 700 mbsf
Total core recovered: 139.4 m (61.8 %)
FMS Pass 1: 148-657 mbsf
FMS Pass 2: 148-657 mbsf
Water depth (from logs): 2786 mbrf
Magnetic declination: -9.253186°
he 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 Leg 164
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.
The FMS images in Hole 995B are of moderate quality, due to
the enlarged and irregular borehole. Hole conditions are partially degraded
above 515 mbsf (except a few sections). Large conductive features are often
associated with hole size variations (e.g., 160-180 mbsf interval), thus any
interpretation of FMS images must be done in close connection with caliper
data.
Locally, the images allow for characterization of
sedimentologic and structural variations. Some intervals (270-300, 380-420,
540-550, mbsf) show conductive, 20 cm thick layers (dark) in a resistive matrix
(light). The dip of these layers is moderate, mainly oriented to the northeast.
High angle to vertical fractures are well identified in some specific intervals
at the bottom of the hole (for example 380-400 and 515-516, mbsf). In some
cases, the electrical images show a mottled structure (resistive cm scale spots
in a conductive matrix) which is typical of bioturbated sediments (for instance
at 515, 580 and 611 mbsf).
Image
Processing
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:
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.
For further information or questions about the processing,
please contact:
Cristina Broglia
Phone: 845-365-8343
Fax: 845-365-3182
E-mail: Cristina Broglia