1 زمینشناسی و معدن:: لایه های رسوبی
change in orientation (tilt- ing) of the once flat-lying sedimentary layers and is called rotation. When flat-lying sedimentary layers are uplifted and tilted, their orientations change, but their shapes are often retained. Anticlines occur when compres- sional stresses squeeze sedimentary layers into arch-like folds. The inclined strata shown in Figure 10.14 once extended over the sedimentary layers now Strike and dip can be used to describe the orienta- tion of sedimentary layers, dikes, joints, and other planar structures, in addition to faults.
واژگان شبکه مترجمین ایران