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Remagnetizations and thrusting in the Idaho-Wyoming Overthrust Belt

✍ Scribed by McWhinnie, S. T.; Van Der Pluijm, Ben A.; Van Der Voo, Rob


Book ID
118671866
Publisher
American Geophysical Union
Year
1990
Tongue
English
Weight
916 KB
Volume
95
Category
Article
ISSN
0148-0227

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The external massifs along the Appalachian orogen include Precambrian basement rocks with attached cover. To the northwest (cratonward), in the Appalachian foreland fold and thrust belt, Palaeozoic sedimentary rocks, but no basement rocks, are exposed; that belt was the subject of the classic debate