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1)  ultra-unit of Yan Jiahe
颜家河超单元
2)  Xiaohe ultra-unit
小河超单元
1.
Both these two units are merged into Xiaohe ultra-unit from the structural evolution.
采用岩石谱系单位的划分原则,依结构演化序列将小河岩体划分为甘沟、后沟两个单元,归并为小河超单元。
3)  Guojialing super-unit
郭家岭超单元
1.
The proto-rock of Linglong and Guojialing super-unit granites is the same of metamorphic rocks of Jiaodong group.
玲珑、郭家岭超单元花岗岩的源岩均为胶东岩群变质岩;玲珑超单元花岗岩表现出岩石的不均匀性,其成因为原地、半原地交代-重熔型花岗岩;郭家岭超单元花岗岩则属于有幔源物质参入的同熔型花岗岩。
4)  Liujiapuzi ultra unit
刘家堡子超单元
1.
Liujiapuzi ultra unit emplaced in Paleo Proterozoic,which the U Pb concordant isotopic age is determined to be 2 046.
刘家堡子超单元同位素锆石U- Pb 一致线年龄值为2 046。
5)  unit-superunit
单元-超单元
1.
Basing on the study about the unit-superunits of granites, the authors divide the member of Laiyuan-Badaling batholith, discuss the main characteristics of the unit-superunits, and point out that this member of .
本文从花岗岩类单元-起单元入手,对涞源-八达岭岩基段进行了划分,探讨了单元-超单元的主要特征,指出本岩基段是在太平洋板块俯冲机制下走滑造山作用的结果,岩浆来源于下地壳未经地表地质作用的深变质火山岩的部分熔融,并有地幔衍生岩浆的混合。
6)  unit reach
单元河段
1.
The Main stream and tributaries above Cuntan Station were separated into many reaches according to the spread time of flow,and every reach is separated into many unit reaches.
按照河段流量传播时间将寸滩以上干、支流划分为若干子河段,各子河段按照计算时段长分成若干单元河段,各单元河段区间降雨径流预报采用水箱模型,河道流量演算采用连续马斯京根法。
2.
The main stream and tributaries above the inflow reservoir station Cuntan were divided into several sub-reaches according to the propagation time of flow,and the sub-reaches were divided into unit reaches according to the calculation time interval.
按照河段流量传播时间将入库站(寸滩)以上干、支流划分为若干子河段,各子河段按照计算时段长分成若干单元河段,各单元河段区间降雨径流预报采用水箱模型,河道流量演算采用连续马斯京根法。
补充资料:胡笳歌,送颜真卿使赴河陇
【诗文】:
君不闻胡笳声最悲,紫髯绿眼胡人吹。吹之一曲犹未了,
愁杀楼兰征戍儿。凉秋八月萧关道,北风吹断天山草。
昆仑山南月欲斜,胡人向月吹胡笳。胡笳怨兮将送君,
秦山遥望陇山云。边城夜夜多愁梦,向月胡笳谁喜闻。



【注释】:



【出处】:
全唐诗:卷199_13
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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