| Environments | PYTHON :: EASI :: MODELER |
| Batch Mode | Yes |
| Quick links | Description :: Parameters :: Parameter descriptions :: Details :: Algorithm :: Related |
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| Name | Type | Length | Value range |
|---|---|---|---|
| Input: Input potential field channels * | Raster port | 1 - 1 | |
| Output: Output filtered image channel * | Raster port | 1 - 1 | |
| Height (Z level) * | Float | 1 - 1 | |
| Report | String | 0 - 192 | See parameter description |
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Input: Input potential field channels
Specifies the input channels containing the potential fields to use in the transformation.
Output: Output filtered image channel
Specifies the output channel to receive the filtered image data.
Height (Z level)
Specifies the height at which to stop the transformation. Positive and negative values for this parameter correspond to upward and downward continuation, respectively. Values must be provided in the same units as the pixel size (usually meters).
Report
Specifies where to direct the generated report.
Available options are:
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FCONT computes upward/downward continuation of a potential field in the input file. The filter is applied in the frequency domain. A 2-D Fourier transformation is first applied to the image. After filtering, the image is transformed back to the spatial domain.
This function is most efficient if the input window has dimensions of a power of 2; otherwise, FCONT must pad extra rows and columns to force the image dimensions a power of 2.
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The input image is first transformed to the frequency domain using a 2-D Fast Fourier transformation (FFT). The dimensions of the transformed image are a power of 2 and are at least as large as the input image dimensions. After applying the filter, the frequency image is transformed back to the spatial domain and truncated to the input image size.
The upward/downward continuation filter has the following form:
exp(-2 PI sqrt(u*u + v*v) ZL)
where u, v are the frequency components. The resolution of u, v are given as:
Delta_u = 1/(SizeU * Delta_x)
Delta_v = 1/(SizeV * Delta_y)
Due to a limitation in the theory, the computed continuation may differ from the actual field measurement at the desired level by a factor which is close to 1. This factor is a constant for the entire potential field at the given level. But if multiple sources with different depths exist, the factor varies.
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