您要查找的是不是:
- CHARACTERISTICS OF SEGMENTS OF SURFACE RUPTURES OF STRONG EARTHQUAKES ALONG THE EAST KUNLUN ACTIVE FAULT ZONE 东昆仑活动断裂带强震地表破裂分段特征
- East Kunlun active fault zone 东昆仑活动断裂
- The East Kunlun active fault is an important NWW-trending boundary fault on the northeastern margin of the Qinghai-Xizang(Tibet) Plateau. 东昆仑活动断裂是青藏高原东北部一条重要的NWW向边界断裂。
- The East Kunlun active fault is an important WNW-trending boundary fault on the northeastern margin of the Qinghai-Tibet Plateau. 东昆仑活动断裂是青藏高原东北缘一条重要的NWW向边界断裂。
- 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
- 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
- Palaeo-earthquake Study on the Maqu Fault of East Kunlun Active Fault 东昆仑断裂带东段玛曲断裂古地震初步研究
- STUDY ON THE ELASTIC STRESS TRIGGERING AMONG THE LARGE EARTHQUAKES IN EASTERN KUNLUN ACTIVE FAULT ZONE 东昆仑活动断裂带大地震之间的弹性应力触发研究
- Characteristics of the activity of the Maqu segment of the East Kunlun active fault belt and its eastward extension 东昆仑活动断裂带玛曲段活动特征及其东延
- Study on characteristics of new activity and Holocene slip rate along Maqu fault of East Kunlun Active Fault 东昆仑断裂带东段玛曲断裂新活动特征及全新世滑动速率研究
- Seismological Bureau of Qinghai Province, Institute of Crustal Deformation, China Seismological Bureau. 1999. TheActive East Kunlun 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
- the East Kunlun active fauh zone 东昆仑活动断裂带
- 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 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 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。