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- 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。
- Institute of Geology,SSB.1990.The Haiyuan active fault zone[M].Seismological Press,Beijing (in Chinese). 国家地震局地质研究所.;1990
- Lanzhou Institute of Seismology, SSB. 1992. The Changma Active Fault Zone [M]. Seismological Press, Beijing. 207 (in Chinese). 国家地震局兰州地震研究所.;1992
- Project Group of the Altun Active Fault Zone of State Seismological Bureau.1992. The Altun Active Fault Zone [M].Seismological Press, Beijing. 国家地震局阿尔金活动断裂带课题组.;1992
- Institute of Geology,State Seismological Bureau,Seimological Bureau of Ningxia Hui Autonomous Region.1990.The Haiyuan active fault zone[M].Seismological Press,Beijing(in Chinese). [1]国家地震局地质研究所;宁夏回族自治区地震局.;1990
- 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。
- Earthquake Administration of Sichuan Province, Institute of Crust Dynamics, China Earthquake Administration. 1999. Eastern Kunlun active fault zone [M]. Seismological Press, Beijing (in Chinese). 青海省地震局;中国地震局地壳应力研究所.;1999
- Seismological Bureau of Qinghai Province, Institute of Crustal Dynamics, China Seismological Bureau. 1999. The Eastern Kunlun Active Fault Zone [M]. Seismological Press, Beijing (in Chinese). 青海省地震局;中国地震局地壳应力研究所.;1999
- Institute of Geology, State Seismological Bureau, Seismological Bureau of Ningxia Hui Autonomous Region. 1990. The Haiyuan Active Fault Zone [M]. Seismological Press, Beijing (in Chinese). 国家地震局地质研究所;宁夏回族自治区地震局.;1990
- Seismological Bureau of Qinghai Province, Institute of Crustal Dynamics of China Seismological Bureau. 1999. The Eastern Kunlun Active Fault Zone [M]. Seismological Press, Beijing (in Chinese). 青海省地震局;中国地震局地壳应力研究所.;1999
- Institute of Geology, State Seismological Bureau, Seismological Bureau of Ningxia Hui Autonomous Region. 1990. The Haiyuan Active Fault Zone [M]. Seismological Press,Beijing.286 (in Chinese). 国家地震局地质研究所;宁夏回族自治区地震局.;1990
- Measuring stress changes within seismically active fault zones has been a long-sought goal of seismology. 测量活动地震断裂带内的应力变化是地震学的长期努力目标。
- The electrical resistivity tomography survey was conducted to detect the active faults along the Tanlu fault zone in Weifang, Shandong province. 摘要在城市活断层调查中，利用电阻率二维层析成像测量方法，对郯庐断裂带山东潍坊段的地震活断层进行了探测试验，取得了较理想的勘探效果。
- Seismological and geodesic observations indicate that slow slip, usually occurs in active fault zones beneath the seismogenic depth, and results in transient ground motion. 摘要观测表明，慢滑移事件通常发生在活动断裂带内，为发震层之下的短暂滑移，能够造成地表的瞬态运动。
- Because of the hazards made by seismic activity, at present more attention has been paid to the design of buried pipelines passing through active fault zone both at home and abroad. 由于地震活动的危害,国内外目前对穿过活动断层区埋地管道的设计均十分重视。
- The Daliang Mountain fault zone is spread out in near SN or NNW in Daliang Mountain hinterland east of the Anning River and Zemu River faults and is through Holocene active fault connecting Xianshui River and Xiaojiang faults,with total length of 280 km. 大凉山断裂带呈近南北向或北北西展布于安宁河、则木河断裂东侧的大凉山腹地 ,是一条连接鲜水河、小江断裂的贯通性全新世活动断裂 ,全长约 2 80km。
- FENG Xian-yue. 1982. The Altun Tagh Fault zone [A]. In: Professional Committee of Seismogeology, Seismological Society of China (ed). Active Faults in China. Seismological Press, Beijing (in Chinese). 冯先岳.;1982
- ACTIVE FAULT SURVEY ON THE TANLU FAULT ZONE IN LAIZHOU BAY 莱州湾海域郯庐断裂带活断层探测
- RED RIVER ACTIVE FAULT ZONE IN NORTHWESTERN SOUTH CHINA SEA 红河活动断裂带在南海西北部的反映
- RESEARCH ON SLIP RATES OF THE LENGLONGLING ACTIVE FAULT ZONE 冷龙岭活动断裂的滑动速率研究
