Airborne Gravity 2010 - Geoscience Australia
Airborne Gravity 2010 - Geoscience Australia
Airborne Gravity 2010 - Geoscience Australia
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<strong>Airborne</strong> <strong>Gravity</strong> <strong>2010</strong><br />
elements) at each crossover point was chosen as the function to minimise. This method works quickly<br />
and efficiently and follows the original philosophy exactly. It should be applied after all obvious<br />
“corrugations” have been previously levelled, e.g., with methods similar to the heading correction or<br />
compensation discussed above.<br />
The images in Figure 3 demonstrate the improvements that can be achieved when adding both<br />
heading and loop corrections to actual FTG data.<br />
(a)<br />
Figure 3. Raw FTG data (a) before heading errors have been removed, and (b) after heading and<br />
loop corrections.<br />
Fourier methods<br />
Use is made of a recent exposition of a Fast Fourier Transform (FFT) for quaternions (Moxey et al.,<br />
2002) that uses two complex numbers to represent quaternions. Together with two FFT’s for two of the<br />
three eigenvalues, the Fourier transform of a tensor can be fully described by four complex Fourier<br />
transformations, instead of the five transformations that would be the case if processing tensors on a<br />
component-by-component basis. Standard FFT filtering operations that respect the inherent physical<br />
properties of the data have been implemented for line or grid-based FTG data, including low-pass,<br />
high-pass, band-pass filters and others.<br />
Quantifying the benefit of acquiring FTG over just Tzz<br />
One of many issues in the current debate about the relative merits of gradient systems is how to<br />
quantify the extra benefit of acquiring FTG versus just one or more components. Barnes et al. (<strong>2010</strong>a,<br />
<strong>2010</strong>b) have produced a spreadsheet to perform such comparisons. They correctly point out that it is<br />
not just the line spacing, speed of acquisition and noise floor of the instruments, but also the<br />
processing that greatly influences the ultimate utility of the acquired data. The proposed method is to<br />
integrate 3 tensor components to estimate Tz and compare that estimate to one produced solely from<br />
integrating Tzz. The design of a transfer function in the spectral domain to take 3 inputs and produce 1<br />
output is not covered here, but we routinely and easily accomplish this using the Intrepid software.<br />
Other parts of the methodology needed here are to:<br />
(a) grid Tzz data using standard minimum curvature methods,<br />
(b) grid full tensor data using the new methods of SLERP/MITRE,<br />
(c) integrate both grids to estimate Tz (Figure 4a),<br />
(d) calculate the difference grid to see where/how the amplitude of the signals differs (Figure<br />
4b), and<br />
(e) calculate the difference in the gravity curvature using a local finite difference grid operator.<br />
The spatial coherence of the differences (Figure 4b) and the significant magnitude of the amplitudes in<br />
the histogram of values in this difference grid of Tz values in Figure 5 combine to illustrate the<br />
significant advantage of using the full tensor data at all stages of inversion and interpretation, even if<br />
the hardware noise is worse.<br />
75<br />
(b)