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1·Sand box analog models have been proved to be powerful tools for demonstrating the structural styles of extensional fault systems.

砂箱模拟实验已被证明是研究盆地内部伸展断层系统的有效工具。

2·These structures form an extensional tectonic system that is genetically related to the formation of the detachment fault.

这些构造构成了一个在成因上与拆离断层形成有关的伸展构造体系。

3·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.

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。

4·Extensional fold is an important component part of tectonic deformation in tensional basins, which distributes widely, and mostly belongs to normal fault-related folds.

伸展褶皱是张性盆地区构造变形的重要组成部分，其分布相当普遍，多属于与正断层相关的褶皱。

5·Based on volcanic activities and tectonic evolution, it is suggested that the tilted fault block, sliding structures in extensional setting should be developed in Cretaceous to Cenozoic age.

结合区域火山活动和构造演化认为，该滑动构造为伸展背景下的掀斜断块型，其滑动时间为白垩纪—新生代。

6·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.

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。

7·This model provides a new idea for revealing the internal relationships of complicated fault assemblages in an extensional tectonic system.

该模式为揭示伸展构造系统中复杂断层组合之间的内在联系提供了新的思路。

8·The Early-Middle Jurassic strata were probably deposited in an extensional basin above the Lapeiquan fault.

早中侏罗世地层可能为拉配泉断裂之上的伸展盆地沉积。

9·During extensional activities of Late Cretaceo us to Eogene, intense upwelling of asthenosphere happened under the fault zone, leading to lithospheric necking in pure shear mode1.

断裂带在晚白垩世-早第三纪的伸展活动中，软流圈进行了强烈的上隆，岩石圈出现了显著的细颈化，属于纯剪切伸展模式。

10·The extension of the continental lithosphere that gives rise to extensional basins is generally considered as a shear process on major, gently dipping normal fault.

形成拉伸盆地的大陆岩石圈伸展构造作用，一般认为是沿大型缓倾角正断层（滑脱断层）的剪切作用过程。