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Out-Of-Sequence and Folded Short Thrusts Produced by Protracted Foreland-Thrust-Belt Interactions, SW Montana
New mapping in the SW Montana reentrant of the Cordilleran fold-and-thrust belt in the Tendoy and Beaverhead mountains shows that it is very different in its structure and sedimentology from most thrust belts. (1) Most frontal thrusts are out-of-sequence in their final stages of evolution; (2) the m
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