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

Cover The Geological Structure of the Sunday Lake Area, Gogebic County, Michigan
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.
>V.M

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