新疆民丰县皮什盖-塔勒克勒格断裂带的第四纪活动特征  

QUATERNARY ACTIVITY CHARACTER OF PISHIGAI-TA-LEKELEGE FAULT ZONE IN MINFENG, XINJIANG

作　　者：柏美祥[1] 

机构地区：[1]新疆维吾尔自治区地震局,新疆乌鲁木齐830011

出　　处：《内陆地震》2003年第2期97-100,共4页Inland Earthquake

摘　　要：皮什盖—塔勒克勒格断裂将蓟县系逆掩于第四系之上 ,中更新世之前的西域变动显著 ,现今地震活动不强烈。其分支断裂帕西木断裂在中更新世之后 ,由正断层变为压性断层。The Jixian System thrusts upon the Quaternary System along the Pishigai-Talekelege fault zone in Minfeng, Xinjiang. The Xiyu movement was outstanding before the Middle Pleistocene in this area, while at present the seimic activity is not strong. Its branched fault, the Paximu fault, has changed to compressive fault from tensional one after the Middle Pleistocene.

关 键 词：第四纪活动断裂 不整合面 西域变动 民丰县 

分 类 号：P315.2[天文地球—地震学]