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1)  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.
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.
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。
2)  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。
3)  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。
4)  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
5)  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。
6)  Yishu fault system
沂沭断裂系
1.
The Yishu fault system is the mainly active fault in the China East, which pression movement happened in the late Jurassic caused the invasion of the cala-alkaline magma and the relevant gold mineralization in the Jiaodong area.
沂沭断裂系在晚侏罗世—早白垩世早期期间的挤压作用造成了胶东地区钙碱性岩浆的侵入 ,同时形成了相应的金矿化。
补充资料:淮沭李战役

标题: 淮沭李战役

英文: huaiyin-shuyang-libao, battleof

1947年3月,国民党军在向山东解放区实施重点进攻的同时,为巩固其占领区,以部分正规军和地方保安团队对江苏省中部和北部地区进行“分区清剿”。坚持在苏中、苏北敌后的中国人民解放军华东野战军第11、第12纵队以少数部队就地活动,主力跳到“清剿”圈外,积极打击敌人。4月初国民党军停止“清剿”,退据点线。4月4日,第11纵队向海安、如皋以东李堡、栟茶地区国民党军发起进攻。至7日,攻占据点20余处,歼其整编第49师第79旅1个团又2个营。21日,该纵队转兵北上,攻克东台以北大中集、新丰镇等据点多处,歼第42集团军1200余人。与此同时,第12纵队在地方武装的配合下,于8日在苏北一举收复蒋坝、高良涧,随后在淮阴至沭阳间广泛出击,歼整编第44师及保安团队各一部。经过近1个月地连续作战,共歼国民党军1万余人,收复了苏中、苏北大片失地,牵制了国民党军近20个旅和10万土杂武装,有力地配合了华东野战军主力在山东战场的作战。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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