5.3.1.1 Well-based Data Extraction

This window presents the attributes and/or logs that can be extracted along well path. The output will be presented in table before being used for cross-plot. At least one well must be selected, and one attribute or one log. It is also possible to select only attributes, or only logs.

The well track and time-depth model provide the locations where to extract the data. Values will be vertically extracted along a specially built measured depth axis. This axis is such that the step between two consecutive depth samples is constant but with few jumps, such that the Z difference (time or depth depending on the survey type) between consecutive depths is around the survey default sampling rate. Therefore at shallow level 1 seismic sample can correspond to 4 meters, then 8 meters at intermediate depths, 12, 16 and so on.

3D Data extraction for Well vs. Attributes Cross-Plot

2D Data extraction for Well vs. Attributes Cross-Plot

The following specific extraction parameters are available:

Extract between: It is used to limit the z-range (depth or time) of the data to extract. There are three options supported: Markers, Depth and Time.

If Markers is selected (which is default), the Start/Stop markers should also be selected from the combo boxes that are available below the extract between field.

If Depth is selected in the extract between field, the start/stop (m) field will be toggled on. In the later fields, starting and stopping depth range is typed in to restrict the data extraction into an interval.

Similarly, if Time is selected in the extract between field, the start/stop (ms) field will be toggled on.

Finally, the step-out for extracting both Attributes and Well data samples has to be defined. This can be defined in meters (default), feet (if the survey is in feet) or milliseconds. The Extract in time check box is usually toggled on if you want to define the data extraction step-out in TWT. It is advisable to check this box when extracting data for crossplotting against seismic volumes.