This is an outcrop example of large-scale folding and faulting, most of which are at a scale that would be visible on seismic sections.
Imagine drilling through this horizontally….
This is an outcrop example of large-scale folding and faulting, most of which are at a scale that would be visible on seismic sections. |
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| In the area, there is an early phase of normal
faulting followed by low-angle reverse faulting. The second phase of normal
faulting is related to doming of the area below a thrust surface. Imagine drilling through this horizontally….
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