同生断层也称生长断层、同沉积断层。
The concept of syngenetic fault is known as growth fault or synsedimentary fault.
生长断层常见于墨西哥湾以及其他地壳快速沉陷或拉分的地区。
Growth faults are common in the Gulf of Mexico and in other areas where the crust is subsiding rapidly or being pulled apart.
伸展盆地生长断层上盘的断鼻型圈闭与逆牵引背斜型圈闭一样是油气勘探的主要目标。
The reverse drag anticline traps and the nose shaped high trap in the hanging wall of growth fault in extensional basin are the major targets in oil and gas exploration.
北部为受生长断层控制的陡坡断阶带，以典型的水下扇、浊积扇和扇三角洲近端前缘沉积为主。
But in the north part of the sub-sag, controlled by the syn-sedimentary fault, steep fault-step was developed with mainly deposition of sub-aqueous fan, turbidity fan, and front of fan-delta.
生长断层成长初期具有独特的断面形态，断层两盘在错动过程之中会产生空隙带和闭合带两种应力状态。
Growth faults have special fault plane form in their initial phase during which the displacement of the two blocks creates two kinds of stress states pore belt and sealing belt.
但是，倾角处理还显示出由于复杂生长断层和与之相关的不连续所形成的间隔，这也同DCWI观察到的反射层相一致。
However, the dip processing also indicated several intervals of complex growth faults and associated discontinuities, and these corresponded with the reflectors seen on the DCWI.
这可以由沉积在不平坦的表面所引起，如邻近和覆于礁体构造之上，或靠近一生长断层，或缘于对压实作用不同的敏感性。
This can result from location on an uneven surface, such as near and over a reef structure, or near a growth fault, or from different susceptibility to compaction.
调节带的形成与两条断层的横向生长叠覆及相互作用有关。
The formation of the accommodation zone is related to growth, overlapping and interaction of the two faults.
不同时期徐中断层生长指数图和断裂落差图分析，得出徐中断裂为走滑断层。
Xuzhong fracture is strike-slip faults can be obtained from different periods fault growth index chart and fracture throw figure of Xuzhong fracture.
裂谷盆地半地堑边界正断层的生长可以划分为两种模式：断层简单生长模式和断层生长连锁模式。
The propagation and growth of boundary faults can be divided into 2 types: simple fault propagation pattern and fault growth-linkage pattern.
从构造几何学分析来看，乌夏断裂带发育12种主要的构造样式类型，其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
从构造几何学分析来看，乌夏断裂带发育12种主要的构造样式类型，其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
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