对周边12 - 2煤层的规划开发、断层样式的认识乃至井田应力场分布的研究提供了依据。
It provided references of programming and developing of nearby coal seam No. 12-2, fault extent recognition and even minefield stress pattern distribution research.
泌阳凹陷在区域性引张作用下形成了典型的伸展构造样式——被不同层次断层切割成的一系列复杂断鼻、断块。
Typical extensional structural patterns, cut into a series of complex fault noses and fault blocks by faults of different levels, form under regional extension force in Biyang depression.
早、中侏罗世形成的正断层组合构造样式，可形成一些小规模油气藏。
The structural pattern of the normal fault assemblage that occurred in the Early and Middle Jurassic may have initiated some small-scale petroleum and gas pools.
其中典型盐构造样式有盐核背斜、外来盐、盐枕、盐焊接和断层焊接、盐缩颈、盐成凹陷和“鱼尾”构造。
The typical salt tectonic styles include salt cored anticlines, allochthonous salt, salt pillows, salt (fault) welds, salt necking, salt-associated depressions and "fish-tail" structures.
分析不同方向、不同尺度断层的位移的兼容性进一步论证了构造族系和构造样式的合理性。
The analysis of displacement compatibility between differ attitude and differ scale faults induced to produce the acceptable structural family and styles for complex faulted-block oil-field.
盆地中发育多种构造样式，主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
第三排构造构造幅度较弱，形成时间较晚，大多为断层传播褶皱或突发构造等样式。
The third anticline belt have low structural height and are folded lately in the form of fault propagation folding or pop-up structures.
准噶尔盆地西北缘前陆冲断带构造样式复杂多样，除规模较大的逆断层外，还发育一系列北西向的走滑断层。
The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.
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.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
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