在垂直于原始的(未形变的)层面量测的每层厚度，在岩层褶皱之后仍保持不变的岩石形变。
The deformation of rock layers in which the thickness of each layer, measured perpendicular to initial (undeformed) layering, is maintained after the rock layers have been folded.
同心褶皱保持各岩层的厚度与在原始层理垂直的方向上所测得的相等。
Concentric folding preserves the thickness of each bed as measured perpendicular to original bedding.
根据对库车褶皱冲断带的地面地质调查和地震反射剖面的解释表明，库车褶皱冲断带克拉苏三角带发育垂直构造走向的位移转换构造。
The field observation and seismic data interpretation reveal that the displacement transfer zone is developed in the Kelasu triangle zone, Kuqa thrust-and-fold belts.
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