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|description={{en|1=Figure 9.2. Illustrates a similar structural situation in which the basement as in (Figure 9.1) was uplifted at the same time as sediments were accumulating in a basin which is now juxtaposed against it. The sediment in the basin is shale which is not the sediment expected from the erosion of an adjacent mountain compare (Figure 9.1). This situation implies that these two blocks (shale basin and basement) had a history which is not compatible with their having been formed adjacent to each other.<br />
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|date=2019-02-10 20:24:41<br />
|source=Geological Society of Glasgow<br />
|author=Geological Society of Glasgow<br />
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