Thrust faults can cause repetition of stratigraphic beds in a vertical cross-section. What term describes the resulting pattern?

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Multiple Choice

Thrust faults can cause repetition of stratigraphic beds in a vertical cross-section. What term describes the resulting pattern?

Explanation:
Thrust faults in compressional settings push slices of rock on top of other slices, so in a vertical cross-section the same stratigraphic package can appear more than once as it’s stacked along the fault. This duplication creates a pattern described as a repeated sequence of beds—the same units show up again higher in the section. An unconformity would show a gap where rocks are missing, a syncline is a downfold that bends beds without duplicating them, and a dip-slip anomaly refers to fault offset rather than repeating the same beds.

Thrust faults in compressional settings push slices of rock on top of other slices, so in a vertical cross-section the same stratigraphic package can appear more than once as it’s stacked along the fault. This duplication creates a pattern described as a repeated sequence of beds—the same units show up again higher in the section. An unconformity would show a gap where rocks are missing, a syncline is a downfold that bends beds without duplicating them, and a dip-slip anomaly refers to fault offset rather than repeating the same beds.

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