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- The Huangpo Fault is as the passage - way for its ore fluid and the sub - order NNE - trending fault zone acts as the main host. 黄-破断裂是其主要的导矿构造，其次级低序次NNE向断裂带是主要的容矿构造。
- The coal-accumulating process of the lower Cretaceous ChanglingFormation was formed in a half graben of the NE trending fault zone which posited on theJinJatun Formation andesite. 下白垩统的长岭组聚煤作用形成于金家屯组安山岩上的北东向断陷带之中，聚煤盆地类型以半地堑式为主。
- The NNE trending faults show an echolon arrangement on horizontal.The different tectonic deformation and strata units exist in the both side of the fault zone. 这些断裂在平面上呈雁行状排列,在断层两盘构造变形和地层差异明显并存在伴生的雁列褶皱,在地震剖面可见发育完好的花状构造,因此具有走滑构造特征。
- The fault zone passes through the offshore between the Changdong islands and the Dazhudao island, and consists of a group of NW trending faults, which are dominated by normal and reverse slips with strike-slip component. 该断裂带由一系列北西走向的次级断层组成，主体在长岛至大竹岛之间的海域，多数断层以正断兼有走滑运动为主，部分断层具有逆冲运动性质。
- In the Qifengcha Detiangou gold field,the N S trending and E W trending fault zones are the major ore bearing structural zones,which are characterized by ductile brittle deformation. 向断裂带与E-W向断裂带是崎峰茶-得田沟金矿田内主要赋矿构造带，具有韧-脆性变形特征；
- The Liangshan active fault zone, trending nearly from north to south, lies at the southeast margin of the Qinghai Tibet Plateau, the east side of Xianshuihe Anninghe Zemuhe Xiaojiang fault zone. 凉山近南北向活动构造带位于青藏高原东南边缘鲜水河 -安宁河 -则木河 -小江断裂带中段东侧 ,与鲜水河断裂带左阶雁列 ,与小江断裂带右阶雁列。
- The occurrence of gold bearing quartz vein was controlled by NNE trending faulted zones. 工业矿体由矿化石英脉的富金段组成。
- Formation Era of Altyn Tagh Fault Zone and Contribution of its Strike-Slip to the Uplift of North Tibet Plateau . 阿尔金断裂带的形成时代及其走滑作用对青藏高原北部隆升的贡献.
- There exists a ground rupture zone along north section of the Shunyi-Liangxiang fault zone near Beijing. 沿北京顺义-良乡断裂北段存在地表破裂带。
- Any place within the fault zone could have breakage. 断层带内的任何地方都会有破裂。
- Dongjiangkou and Zhashui rockbodies are located in south side of Shangdan fault zone,which belong to Variscan batholith. 南秦岭东江口、柞水岩体位于南丹断裂带南侧，为华力西期岩基。
- Two groups of faults,the north to east trend faults and the east to west trend faults,crossed horizontally to form 16 oil-bearing blocks. 平面上受北东走向断层和东西走向两组断层夹持形成了“墙角式”的16个含油断块,各断块之间无统一油水界面;
- 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。
- The ore bodies are strictly controlled by SN and NNW trend fault and the wall rocks and the intrusive rocks are involved in the mineralization. 金矿体严格受SN和NNW向断裂控制,围岩和侵入岩参与了成矿作用。
- 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。
- Machaoying strike-slip fault zone which is for med in the middle part of the north of the eastern Qinling is a positive flo wer st ructure. 马超营走滑转换构造带位于二者之间，为一正花状构造带。
- The authors describe the geometry and deformation features of the Machaoying fault zone in the Huaxiong terrane,southern margin of North China Craton. 对华熊地块南部的马超营断裂带的几何样式、组成特征及其变形特点等研究结果表明,马超营断裂带经历了韧性变形和脆性变形期。
- 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。
- It is a collision suture between the Yangtze Block and North China Block during the Indosinian period, a thrust-napping fault zone belonging to the Tethyan regimes in broad sense. 在印支期由于扬子地块与华北地块的碰撞，成为两板块的对接边界，具有逆冲推覆的性质，属广义的特提斯构造域。
- The tin-mineralized north Dayishan granite body is a S-type granitic intrusion emplaced from southeast towards northwest along the Chenzhou-Shaoyang deep-seated fault zone. 大义山花岗岩体北体是矿田锡矿的主要成矿岩体,属燕山晚期“S”型酸性铝过饱和花岗岩,被动侵位于郴州-邵阳深断裂带走滑作用形成的剪切拉张桥区。
