1) Shuhe fracture zone
沭河断裂带
1.
As a middle section of Tanlu fracture zone,Shuhe fracture zone intersects Wulian Qingdao tectonic zone in eastern part of Shandong, which makes up of an image of a reverse “ 入type" .
郯庐断裂带中段沭河断裂带与五莲—青岛构造带在山东东部斜接,二者在遥感图像上组成一个倒“入”字图形。
2) Yishu fault zone
沂沭断裂带
1.
Differential activity within Yishu fault zone and its caus es of formation;
沂沭断裂带内部的差异活动及其成因分析
2.
Based on geological survey,the authors divided the seismogenic rocks in the Yishu fault zone and its periphery into four types,namely,seismite,seismic fault-tectonic rock,seismic volcanic rock and cryptoexplosive-seismic breccias.
将沂沭断裂带及其附近地区的地震成因岩石划分为四种类型,它们是具有地震成因构造的震积岩、震断层构造岩、震火山岩及隐爆地震角砾岩。
3.
In the Yishu fault zone and its surrounding area,seismites have been discovered in four horizons,i.
在沂沭断裂带及其近区,已发现震旦纪石旺庄组、寒武纪馒头组、古近纪朱壁店组和沙河街组四个层位发育震积岩,它们均是具有地震液化脉构造和其它地震成因层内构造的震积岩层。
3) Yi-Shu fault belt
沂沭断裂带
1.
Characteristics of fluid inclusions from two types of gold deposits in central part of Yi-Shu fault belt and their geological significance;
沂沭断裂带中段两种类型金矿流体包裹体特征及其地质意义
4) Yishu fault belt
沂沭断裂带
1.
Longquanzhan gold deposit in Yishui county locates in middle part of Yishu fault belt, which was controlled by Yishui-Tangtou fault.
沂水县龙泉站金矿位于沂沭断裂带中段,受沂水汤头断裂控制。
2.
The management information system for geothermal resources of Yishu fault belt was studied on the basis of Mapinfo software.
山东省沂沭断裂带地热资源管理信息系统是以Mapinfo为平台,通过建立地热信息数据库及软件二次开发,实现对山东沂沭断裂带地区地热资源空间多源信息数据的有效管理。
5) Yishu fault
沂沭断裂带
1.
The faulting characteristics of Yishu fault are analyzed by using the levelling data.
利用跨断层短水准资料分析了沂沭断裂带断层活动特征 ,结果表明 :NNE向的沂沭断裂带与NW向断裂活动性质有所不同 ,沂沭断裂带主要为压性逆断活动 ,北西向断裂带为张性正断活动 ,与地质考察结果基本一致。
2.
Though the research geothermal geological condition,this article found out that the geothermal formation in Linyi segment of Yishu fault zone was relation with the fault,geological structure and magmatic activities.
通过对沂沭断裂带临沂段地热地质条件研究,认为本区地热形成与断裂、构造、岩浆活动相关;通过测温、遥感解译等手段,确定汤头、穆柯寨、芝麻墩地热异常区及地温梯度的空间变化。
6) Yishu Fault
沂沭断裂
1.
Jiaolai Basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -Jimo-Muping Fault.
胶莱盆地是中生代走滑拉分盆地,其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。
2.
They originated in a tectonic setting of strong activity of the Yishu fault.
沂沭断裂中段的石场—中楼一带，存在受北北东向断裂控制的早白垩世莱阳群火山碎屑岩系。
补充资料：沭河栗海
素有“杨柳遮路不知村，绿林深处有人家”的中国板栗之乡，临沭县白旄镇沭河古栗林位于沭河北段东侧的河滩地带，自古就有“沭河栗海”之美誉。它沿河遍布于南起周官庄，北至柳庄村的整个沭河流域。栗海西涉碧水金沙，东望杞柳翻浪，南北长15公里，东西宽数里，总面积10万余亩。约五百万株古栗树，多数为明清时期所植，至今枝繁果盛。栗树最大胸径约2m，最长树龄乃云林观古唐栗，相传系隋唐瓦岗寨首领程咬金亲手所植。因此，当地人称其为“千岁栗祖”。观前有楹联曰：“问四时墨林何处弄来碧水金沙呈画卷，听千岁栗祖眼前正于闲云雅士话苍桑”。
沭河栗海树姿百态，造形奇异，金色柔软的沙地林带上，芳草青青，彩蝶翩翩。春天花放万树；夏时栗林深幽；秋季硕果累累；冬雪鹤鸟竞飞，真乃名符其实的栗海森林。各种桃李杂果相间林中，许多珍稀野生动植物随处可见。栗海文化底蕴深厚，人文趣事传说众多，古代绿林好汉罗成的爱情故事成为美谈。云林观遗址、龙凤栗轶事、钟华山的传说、柳毅庙的晨钟暮鼓，更为古栗海增添了许多神秘的色彩。目前，该栗林被国内知名专家认定为是现代人休闲度假、回归自然和举办各种大型节庆活动的理想佳境。
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