亚肯背斜带在前陆盆地变形机制控制下，以隐伏的顺层滑脱—推覆为特点，褶皱平缓。
Yaken anticline zone controlled by deformation mechanism of foreland basin is characterized by subtle detachment along the formation surface and shows gentle fold.
本文讨论了南阳凹陷东庄地区的构造特征，探讨了东庄地区同生断裂、背斜构造和地堑式断裂的形成机制。本区同生断裂的发育，与沉积中心逐渐南迁密切相关。
Structural characteristics in Dongzhuang area of Nanyang depression are discussed, and the formation mechanism of growth faults, anticline and graben faults is approached in this paper.
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