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What was the Grenville orogeny and crustal assembly?

The Grenville orogeny was a long-lived Mesoproterozoic mountain-building event that played a crucial role in assembling the supercontinent Rodinia. Spanning roughly from 1250 to 980 million years ago, its geological footprint extends across North America, Scotland, and correlates with worldwide orogenic belts under different regional names. Furthermore, the early geologic processes linked to Rodinia's creation trace back over a billion years, forming a foundation for later structures like the Appalachian Mountains.

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