摘要
在昆仑山南部西大滩与东大滩谷地，沿西大滩活动断裂发育大量串珠状斜列分布的地震鼓包，与不同类型的地震破裂、地震楔、地震陡坎和地震凹陷伴生，在探槽剖面表现为全新世砂土层和晚更新世砾石层的背斜褶皱变形；地震鼓包长轴走向290°～300°，与西大滩活动断裂呈10°～20°交角，锐角指示西大滩断裂左旋走滑运动方向。对探槽剖面不同层位的沉积物、断层破碎带和地震崩积楔分别取样，进行热释光和光释光测年，发现西大滩断裂的地震鼓包主要形成于全新世早期，对应于10．2ka BP、8．6～8．7ka BP、7．0ka BP、6．10ka BP4期古地震事件。估算西大滩断裂全新世早期强烈地震的复发周期为0．9～1．7ka，断裂左旋走滑速率为5．3～10．0mm／a，平均约7．7mm／a。全新世晚期西大滩断裂的构造活动性显著减弱，强烈地震向南迁移至库赛湖断裂。
A great deal of pressure ridges distribute along the Xidatan strike-slip fault in en-echelon pattern accompanied by varieties of seismic fractures, seismic wedges, seismic scarps and seismic sag-ponds in the Xidatan and Dongdatan valleys in south Kunlun Mts. of north Tibetan Plateau. Most pressure ridges show anticline deformation of Holocene and Late Pleistocene sediments in trench cross-section with anticline axis trending in 290°-300°. And an angle ranging 10°-20° exists between pressure ridge and main active fault, directing sinistral strike-slip motion of the Xidatan fault. Thermoluminescent （TL） and photoluninescent （OSL） dating were finished for samples from different parts of pressure ridges and seismic fractures. Accoding to TL and OSL dating, 4 paleo-earthquakes occurred and 4 stages of pressure ridges formed in 10.2ka BP, 8. 7ka BP, 7.0ka BP and 6. lka BP respectively in Early Holocene, corresponding to earthquake intervals of 900 1700a and strike-slip rates of 5. 3-0. 0mm/a with average slip rate of 7. 7mm/a of the Xidatan fault. Activity of the Xidatan strike-slip fault became weak since 5.0ka BP, and strong earthquake of Ms≥8.0 seems migrated from Xidatan fault to Kusaihu active fault in south boundary of Kunlun Mts. in Late Holocene.
出处
《地质论评》
CAS
CSCD
北大核心
2006年第1期15-24,i0001,共11页
Geological Review
基金
青藏铁路沿线活动断层调查与监测项目
国际合作项目(编号INDEPTH-IV)
子项目(编号2001CB711001)的部分成果
关键词
地震鼓包
古地震
热释光和光释光测年
西大滩断裂
昆仑山南部
pressure ridge, paleo-earthquake, thermoluminescent and photoluninescent dating, Xidatan strike-slip fault, southern Kunlun Mts.
