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新疆富蕴地震断裂带中南段结构特征
引用本文:柏美祥.新疆富蕴地震断裂带中南段结构特征[J].内陆地震,2002,16(2):126-135.
作者姓名:柏美祥
作者单位:新疆维吾尔自治区地震局,新疆乌鲁木齐,830011
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。

关 键 词:地震断裂带  断裂结构  新疆
文章编号:1001-8956(2002)02-0126-10
修稿时间:2002年3月21日

STRUCTURAL FEATURES IN THE MID-SOUTH SEGMENT OFFUYUN, XINJIANG, EARTHQUAKE FAULT ZONE
BAI Mei,xiang.STRUCTURAL FEATURES IN THE MID-SOUTH SEGMENT OFFUYUN, XINJIANG, EARTHQUAKE FAULT ZONE[J].Inland Earthquake,2002,16(2):126-135.
Authors:BAI Mei  xiang
Abstract: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.
Keywords:Earthquake fault zone  Fault structure  Xinjiang
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