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Hi @CavemanEx, welcome to the forum! This is a common problem with interpolation of airborne geophysics. The main issue is that data are oversampled along flight lines and there no information between the lines. If you interpolate with a small grid spacing to take advantage of the large sampling along lines, the interpolator has to make up data between lines. Most interpolators will try to smooth and decay away from actual data. This is what creates the patterns along flight lines (the many points between lines tend to decay until they get close to another line). There aren't really good solutions to this problem. Some things that can be done:
If it helps, there is this example of how I made a grid of airborne magnetic data for Ensaio: https://www.fatiando.org/ensaio/latest/gallery/lightning-creek-magnetic.html#sphx-glr-gallery-lightning-creek-magnetic-py (this shows the grid and there is a link to the code that generated it). It uses equivalent sources, which are very similar to the gridding in Verde. |
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Awesome, thanks for the reply! This is a great project by the way! I've found it extremely helpful in everything from visualizing and interpreting geophysics to geochemical samples. |
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Great to know @CavemanEx! Please share any work you did using Fatiando under the Show And Tell category here in the forum: https://github.com/orgs/fatiando/discussions/categories/show-and-tell We love learning what people are up to and it can help us plan the development and justify the effort we put into this.
That is a great question that I don't really have a good answer for. I feel that there must be some relationship but I've never seen anything published on this that was convincing. There might be something in variogram analysis that could provide insight but that's as far as I've gone. If you do find something, please share! |
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Hi @CavemanEx, welcome to the forum! This is a common problem with interpolation of airborne geophysics. The main issue is that data are oversampled along flight lines and there no information between the lines. If you interpolate with a small grid spacing to take advantage of the large sampling along lines, the interpolator has to make up data between lines. Most interpolators will try to smooth and decay away from actual data. This is what creates the patterns along flight lines (the many points between lines tend to decay until they get close to another line).
There aren't really good solutions to this problem. Some things that can be done: