Download Multi-scale edge detection wizard (T44a)
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INTREPID User Manual Library | Help | Top Multi-scale edge detection wizard (T44a) 2 | Back | processes for magnetic data. FTG data processing follows the same workflow in this tool, including upward continuation, point picking maximum gradients, joining the points into worms, formation of linears, and now the 3D surface clustering algorithm. WARNING - Whilst Geodetic grids are supported, you can get into more trouble than it may be worth. Note, we are upwards continuing, assuming a planar or flat world. The units of upwards continuation are meters. For the Geodetic case, we internally make these equivalent decimal degrees to follow your wishes. Also, as the points are located to form the WORMS, the tolerances are stretched. The output projection of derived datsets follows from the input grid. A Lambert Conic Conformal projection is often used when a continental or very large regional extent is involved. In this chapter: How to use this chapter Overview of the Multi-scale edge detection wizard process Using the Multi-scale edge detection wizard—overview (interactive only) Step 1—Specify input dataset, scalar TMI grid example Step 2—Pre-process and filter Step 3—Calculate edge points Step 4—Group edge points into 'worms' Step 5 - Calculate linears Step 7—Export results Specifying input and output files All further options are common to the previous tutorial descriptions. The next image shows the stacked “worms” for this dataset in the Intrepid Visual tool. The amplitude field is used to colour code the polylines. The deeper, more important contacts, are shown in red. Apply Exit Task specification (.job) files Finding out more about spectral domain operations Glossary References Library | Help | Top © 2012 Intrepid Geophysics | Back |