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- An unconformity in which older strata dip at different angle from that of younger strata.
Source: Leet, L. Don. 1982. Physical Geology, 6th Edition. Englewood Cliffs, NJ: Prentice-Hall
- An unconformity in which the older underlying strata dip at a different angle (generally steeper) than the younger overlying strata. See also: disconformity
Source: Dictionary of Mining, Mineral, and Related Terms
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