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| Fig. 5.7: Map view of a segment the South Mountain Anticline showing that the distribution of strain is roughly independent of position along strike, suggesting the validity of a two-dimensional approximation. Identical ellipses only indicate the trend of the long axis of the strain ellipse; the axial ratio in the cross-section is plotted by each. Axial ratios are comparable in strike-parallel belts. Reprinted from (Cloos, 1971, Plate 1) with permission of The Johns Hopkins University Press. | ||||
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