同生构造控制了盆地的形成、沉积及演化。
Syngenetic structures controlled the basin 's forming, settling and evolving.
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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