1) fault zone trapped waves
断层围陷波
1.
As the first application of fault zone trapped waves to the active fault exploration in urban areas,an experiment aimed at Tangxi Fault of Taihang Mtns.
作为断层围陷波方法在城市活断层探测中的首次尝试,我们针对太行山山前断裂带南段的汤西断裂开展了爆炸震源的观测试验。
2.
The observation of the fault zone trapped waves was conducted using a seismic line with dense receivers across surface rupture zone of the M =8.
1级地震进行了断层围陷波的观测实验。
3.
The observational results show that the fault zone trapped waves from the fractured zone of Wenchuan Ms 8.
该断层围陷波测线横跨断层,以地震探槽为大致中点,沿NW-SE方向两端延伸,测线长约400m。
2) fault depressions
断陷层系
1.
Middle and large oil/gas fields are largely distributed in the deep fault depressions along the two sides of NNE Sunwu-shuangliao lithosphere fault crossing the central part of Songliao basin.
松辽盆地断陷层系大、中型油气田主要分布于贯穿松辽盆地中央区域的北北东向孙吴-双辽岩石圈断裂两侧的深断陷之中。
3) fault interpretation pitfall
断层陷阱
4) faulted sequence
断陷层序
1.
There are two successions of source rocks in the northern Songliao Basin,which are dark shale and coal developed in the faulted sequences of Shahezi(K_1s) and Yingcheng(K_(1)y) Formation and dark shale in the depressed sequences of Qingshankou(K_2qn) and Nenjiang(K_(2)n) Formation.
松辽盆地滨北地区目前已发现深层和中浅层两套烃源岩:深层断陷层序的沙河子组和营城组发育的暗色泥岩和含煤地层及中浅层坳陷层序发育的青山口组和嫩江组暗色泥岩。
5) fault depression
断层坳陷
6) fault subsidence
断层沉陷
补充资料:陷围
1.犹言包围圈。
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