The Geological Structure of the Sunday Lake Area, Gogebic County, Michigan

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The Geological Structure of the Sunday Lake Area, Gogebic County, Michigan
Pearsall, William Gilchrist
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Figures 5 and 6 are folds whose axial lines pitch about 55® S.E., and whose axial planes dip about 50® ]?.E. It will he seen hy the attitude of the folds that, while the formations were F:till flat-lying "beds from what was originally the southeast direction, they had a tendency to come up over beds to the northwest, as in Fig.
5a, giving a differential movement of the kind diown by the arrov/s and the strain ellipsoid. This would indicate that the formations had been subjected to a pt^essurc a
...cting in a southoast-northv/est direction, resulting in folding and shortening. The thrust would bo from the southeast rather than from the northwect because the pitch of the axial lines is toward the southeast.
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