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- Longmenshan fault zone, being collision boundary of Chuan Qing with Yangtze block,is charactered by especial tectonic and segmentation. 龙门山断裂构造带作为川青地块与扬子地块的碰撞边界,具有特殊的构造性质及明显的分段性。
- Seismogenic structure is constructed with the central Longmenshan fault zone, squeezed under stress from southwest to the north east thrust movement; 发震构造是龙门山构造带中央断裂带，在挤压应力作用下，由南西向北东逆冲运动；
- Longmenshan fault zone 龙门山断裂带
- the Longmenshan fault zone 龙门山断裂带
- The reasearch area is delimitated by Xianshuihe Fault and Longmenshan Fault. 坝区外围还存在象抚边河断裂这样的近期强烈活动过的断层等。
- Longmenshan faults zone 龙门山断裂带
- Any place within the fault zone could have breakage. 断层带内的任何地方都会有破裂。
- The Tan Lu Fault zone experienced intense thrusting since Neogene. 郯庐断裂带于新近纪以来呈现强烈的逆冲活动,使得先存的伸展性断层产生了一系列逆冲反转构造。
- As it is a fault zone, the landforms here have special features. 由于是断裂带，这里的地貌特征很特别。
- The earthquake’s epicenter and focal-mechanism are consistent with it having occurred as the result of movement on the Longmenshan fault or a tectonically related fault. 这次地震的震中及震源机制是一致的，它有发生的结果，运动对龙门山故障，或构造有关的故障。
- The earthquake's epicenter and focal-mechanism are consistent with it having occurred as the result of movement on the Longmenshan fault or a tectonically related fault. 震中和震源机制和龙门山断层或与该断层相关的地质构造运动结果的发生是一致的。
- The gouge of the fault zone may extend to depths of some kilometers. 断层区的断层泥可能伸展到若干公里的深度。
- Design and Construction of Pile Foundation in a Rich Water Fault Zone. 富水断裂带上桩基设计与施工。
- The metallogenesis is strictly controlled by NE-trending shear fault zone. 成矿严格受NE向剪切断裂带控制。
- Variations in rock type and structure in the fault zone would entail variations in slippage rate along the trace. 断层区的岩石类型和构造的不同将会引起沿断痕滑动的速率的变化。
- SUN Yan, HAN Ke-cong. 1985. Division of Tectonites in Fault Zone [M]. Science Press, Beijing (in Chinese). 孙岩;韩克从.;1985
- When a break occurs the fault zone can be retrieved from storage and this enables higher warping speeds to be used. 一旦发生断头,断头所在的纱段可以从储存系统中退出。这种装置使高速整经成为可能。
- The active fault zone in the northern fringe of Hami Basin strikes NNW, 180 km longdisjointedly. 哈密盆地北线活动断裂带走向北西西，断续长180km。
- The main shock occurred on the dextral obduction-type fault zone and the hypocenter depth was about 15km . 汶川地震的主震发生在具有右旋性质的仰冲型断层带上，震源深度为15公里左右。
- The northeastward Xiangshui fault zone in this area is the main rock-control and ore-control structure. 区内北东向响水断裂带是主要的控岩和控矿构造。
