What are megaterraces in very large impact basins?

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In the study of meteorite craters, megaterraces are defined as discrete, inward-facing, and widely spaced faults that develop well outside the initial excavation cavity of a crater.1

These features are specific to very large impact structures known as impact basins. While smaller complex craters feature terraces formed by downward faulting along the inner rim of the initial cavity, the formation of megaterraces represents a more extensive structural modification associated with the largest scale of impact events.1