1) Tales of Hedong
河东记
2) Hedong
河东
1.
This paper discussed the Hedong town.
河东,顾名思义指河水以东,唐代的河东地区包括今天的山西全省以及河北西北部内外长城之间的地区。
2.
There are three different views on the native place of Chen Yuanguang which are the places of Hedong,Jieyang and Gushi.
陈元光里籍有河东说、揭阳说、固始说三种,而河东是陈元光家族的郡望,揭阳也不过是广东志书从"扬善颂贤"的感情出发硬拉名人的结果,而固始说不仅有可信的文献依据,而且从唐初全国形势、军事制度以及固始人口状况来分析,也最具合理性。
4) Donghe sandstone
东河砂岩
1.
Sequence boundary types and logging identification of Donghe sandstone in HD4 oilfield,Tarim Basin;
塔里木盆地哈得4油田东河砂岩层序地层界面类型及测井识别方法
2.
Using diagenetic facies to analyze heterogeneous reservoir of Donghe sandstone of east slope of Lunnan,Tarim Basin;
用成岩岩相分析法剖析轮南东斜坡东河砂岩非均质性储集层
3.
Characteristics of Carbonate Cement in Donghe Sandstone and Its Effect on Reservoir;
东河砂岩中碳酸盐胶结物特征及对储层的影响
5) Hedong coalfield
河东煤田
1.
Research on gas controlling by tectonism of center and the south of Hedong coalfield;
河东煤田中南部构造控气研究
2.
This paper deals with the coal-bearing measures of the Taiyuan Formation (C2) in the Fugu - Baode mine of the Hedong coalfield (the Northwest China) on the basis of the sedimentary characteristics of a main sandstone body (the Qiaotou sandstone body), including its mineralogy, petrology, textures, sedimentary structures, paleocurrents and spatial geometry.
本文对我国河东煤田府谷-保德矿区太原组(C_2)下段的骨架砂体(桥头砂岩)的几何形态、垂直层序类型、岩石学和矿物学特点、概率曲线特征、沉积构造类型及其组合特点、古水流特征进行了细致的观察与分析,结合该骨架砂体对下伏m_(13)厚煤层的冲刷样式,对其沉积环境和发育期的盆地独特的同沉积期的古构造背景进行了判断。
3.
The authors discover, in the Carboniferous-Permian coal reservoir in Hedong coalfield, Shanxi Province, two groups of joints similar to the traditional exo_joints in scale and to the cleat in occurrence, joint feature, growth carrier and other features.
在山西河东煤田石炭、二叠纪煤储层中发现规模类似于传统外生节理，而产状、节理面特征及发育载体等其他特征与内生裂隙极为相似的两组节理。
6) East Liaohe River
东辽河
1.
Environmental Characteristics of the Atrazine in the Waters in East Liaohe River Basin;
东辽河流域地表水体中Atrazine的环境特征
2.
Analysis of unanimity for water resources evaluation in East liaohe river;
东辽河水资源评价的一致性分析
3.
Based on the analysis of the primary theory of ESW, the evolution and variation of the ESW in the East Liaohe river basin(ELRB) are analyzed with the key desktop of GIS.
在分析水生态空间基础理论的基础上,以东辽河流域为例,以GIS技术为关键的数据处理平台,分析了流域地表水生态空间的演化分异。
补充资料：病中闻河东公乐营置酒口占寄上
【诗文】：
闻驻行春旆，中途赏物华。缘忧武昌柳，遂忆洛阳花。
嵇鹤元无对，荀龙不在夸。只将沧海月，长压赤城霞。
兴欲倾燕馆，欢终到习家。风长应侧帽，路隘岂容车。
楼迥波窥锦，窗虚日弄纱。锁门金了鸟，展障玉鸦叉。
舞妙从兼楚，歌能莫杂巴。必投潘岳果，谁掺祢衡挝。
刻烛当时忝，传杯此夕赊。可怜漳浦卧，愁绪独如麻。
【注释】：
【出处】：
全唐诗：卷541-101
闻驻行春旆，中途赏物华。缘忧武昌柳，遂忆洛阳花。
嵇鹤元无对，荀龙不在夸。只将沧海月，长压赤城霞。
兴欲倾燕馆，欢终到习家。风长应侧帽，路隘岂容车。
楼迥波窥锦，窗虚日弄纱。锁门金了鸟，展障玉鸦叉。
舞妙从兼楚，歌能莫杂巴。必投潘岳果，谁掺祢衡挝。
刻烛当时忝，传杯此夕赊。可怜漳浦卧，愁绪独如麻。
【注释】：
【出处】：
全唐诗：卷541-101
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