真倾斜
Structure form in time domain seismic cross-section often distort, such as high point deviate, attitude of stratum ( direction and angle of dip) deform away from the true.
时间域地震剖面上的构造形态时常发生畸变,例如高点偏离,地层产状(倾向、倾角)失真等。
If the true dip line of one or two joint planes plot within a sliding zone of double-faced slope, a double-faced sliding failure can be possible.
如果有一两个节理面真倾向线落在滑动区内,滑动破坏才可能发生。
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