... | ... | @@ -198,26 +198,23 @@ Example 1: |
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In the first example, a model with Gaussian top topography and gradient velocity is built, and the source is selected as the explosive source in the middle. The seismic wavefield snapshots are taken and the seismograms are recorded by two stations symmetrically located on the free surface.
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![Example 1: model](https://github.com/diasgeo/elm/blob/master/elm2d/outreach/example1_1.png)
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![example1_1](uploads/38aa8d88b18f0f36ee797f4162abebdb/example1_1.png)
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Fig 1-1: The model deployment.
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![Example 1: snapshots](https://github.com/diasgeo/elm/blob/master/elm2d/outreach/example1_3.gif)
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Fig 1-1: The model deployment.
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![example1_3](uploads/80b7f077fd98c3aa1c7240041495313a/example1_3.gif)
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Fig 1-2: Animation of seismic wavefield.
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![Example 1: seismogram]
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(https://github.com/diasgeo/elm/blob/master/elm2d/outreach/example1_2.png)
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![Example 1: seismogram] ![example1_2](uploads/3305b7c4a8d9967fb391e8df3a869fa6/example1_2.png)
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Fig 1-3: Seismograms.
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![example1_3](uploads/c5fcbacd9c59b811103b3a18cd53791f/example1_3.gif)
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Example 2:
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In the second example, 3 different type of sources are taken in the homogeneous model, e.g., a single force in X direction, an explosive source, and a dip-slip moment tensor source. The seismic wavefield snapshots are taken at the same time.
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![Example 2: snapshots](https://github.com/diasgeo/elm/blob/master/elm2d/outreach/example2.png)
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![example2](uploads/0ad244f4e7ebba4655d54a1b771e45dc/example2.png)
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Fig 2: Snapshots of seismic wavefield.
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# Reference
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