新疆富蕴地震断裂带中南段结构特征  

STRUCTURAL FEATURES IN THE MID-SOUTH SEGMENT OF FUYUN, XINJIANG, EARTHQUAKE FAULT ZONE

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》2002年第2期126-135,共10页Inland Earthquake

摘　　要：新疆富蕴地震断裂带中南段受北北西走向可可托海—二台活动断裂和东侧北西走向玛因鄂博等活动断裂所控制 ,形成“爪”形 ,左阶帚状 ,右阶弧形 ,反 S形半透镜状和肘状构造。The mid south segment of Fuyun, Xinjiang, earthquake fault zone is a part of main strike slip segment of the fault zone. Controlled by the inherited right lateral movement of NNW trending Keketuohai Ertai active fault belt and NW trending Mayinebo active fault, there are paw shaped, left stepped broom shaped, right stepped arcuate, reversed S shaped semi lens and elbow shaped structures forming in the mid south segment of the fault zone.

关 键 词：地震断裂带 断裂结构 新疆 左阶帚状 肘状构造 反S形半透镜状 

分 类 号：P315.2[天文地球—地震学]