1) Xiannushan fault zone
仙女山断裂带
1.
Xiannushan fault zone is one of the regional fault structures at western Hubei province.
文章在概略介绍仙女山断裂带所处的大地构造位置、展布特征、组合关系基础上,用详实的材料,逐一分析了荒口—腰店子、腰店子—将军垭、将军垭—卜庄河及尹家湾—黄垭畔、黄垭畔—贾家店长江南北两岸各段的断裂构造形迹特征、力学性质和交切关系。
2) Xiannushan fault zone
仙女山断裂
1.
The results show that the activity of Xiannushan fault zone nearby the reservoir has changed and tilt field around the reservoir has changed micro-dynamically because of reservoir impounding, the tilt field in lower reaches of reservoir has no obvious change.
为研究三峡水库蓄水所引起的库区地壳形变和断层活动,运用小波变换分析和处理了大坝附近两个定点形变台(周坪台和宜昌台)的倾斜观测数据,发现蓄水后库区仙女山断裂带的活动发生了一些变化,库区周围的倾斜场发生微动态变化,库区下游区域的倾斜场没有发生明显的变化。
2.
Activity of Xiannushan fault zone near reservoir has changed,it means that the impoundment has lead to micro-dynamic variations of tilt field in the reservoir and adjacent area.
结果显示:水管倾斜仪对蓄水效应有较好的响应,主要在数据的长趋势项(周期稍长的细节层)有反映;三峡库区附近的仙女山断裂带的活动发生了一些变化,说明蓄水使库区周围的倾斜场发生了微动态变化。
3) The Xiannufeng and Jiuwanxi fault zones
九湾溪和仙女山断裂带
4) Xiannushan fault
仙女山断层
1.
Through the geologic drawing of fault zone and microscopic analysis of tectonic rook in the deformation monitoring caves of the Xiannushan fault and the Jiuwanxi fault, the samples of fault mud and calcite were selected and dated age by thermoluminescent (TL).
同时对洞外披覆跨仙女山断层上的第四纪河流冲积物、断层一侧周坪河谷底上第四纪湖相纹泥夹碳化木及披覆跨九湾溪断层上的第四纪崩滑堆积体中滑带土进行测年。
5) Changliu-Xiangou fault zone
长流-仙沟断裂带
1.
The Holocene volcanic activity of the Leihuling Group are distributed mainly along the Changliu-Xiangou fault zone in the Shishan-Yongxing area Many large-scale faults are found in the base-surge deposits which are created by phreatomagmatic eruptions in Shishan area.
琼北地区的火山活动以裂隙喷溢为主,晚更新世道堂期的射气岩浆喷发形成了众多的低平火山口,全新世雷虎岭期火山口主要分布于石山、永兴一带,沿NW向长流-仙沟断裂带分布。
6) back range faults
后山断裂带
1.
Late Quaternary kinematic characteristic of the back range faults at the Middle Longmenshan fault zone;
龙门山中段后山断裂带晚第四纪运动特征
补充资料：仙女
1.女仙人。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条