摘要
对水库近场区内的多条活动断裂研究认为 :区域性北轮台断裂具分段性 ,水库所在的西部断裂全新世以来未活动 ;全新世活动的东却勒塔格断裂向东延伸至二八台河以西 ;库区土尸洛克背斜核部有全新世断裂 ,但对水库影响不大 ;牙哈背斜北翼发现 1 0 km左右的断裂陡坎 。
There are many active faults at the area of the Wuyi reservoir, Luntai,Xinjiang. The research on the faults shows that the Beiluntai fault is in segments. The faults the west of the reservoir haven't activity since Holocene. The Dongqueletage fault which had activity in Holocene extends to the west of the Erbatai River toward east. In the core of the Tushiluoke anticline, the fault in Holocene was found. And about 10 km long fault scarp was found at the north flank of the Yaha anticline.
出处
《内陆地震》
2003年第1期27-32,共6页
Inland Earthquake
关键词
活动断裂
水库
全新世
库车坳陷
South Tianshan
Active fault
Kuche depression
Fault scarp
