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A high level of satisfaction with one's work is most likely to be reported by those who frequently experience
Fold and Thrust Belt
A series of mountainous folds and thrust faults that develop near convergent tectonic plate boundaries, where one plate is forced over another.
Foreland Basin
A foreland basin is a structural depression that forms adjacent to a mountain range due to flexural subsidence, filling with sediments eroded from the associated orogeny (mountain-building process).
Back-Arc Rifting
A geological process in which the crust behind a volcanic arc stretches and thins, often leading to the formation of a new ocean basin.
Michigan Basin
A geological basin in the United States characterized by layers of sedimentary rock, indicative of its history as an ancient sea bed.
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