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1)  dong he oilfield
东河CⅢ~1岩性段
2)  Donghe sandstone interval
东河砂岩段
1.
The Bioclastic Limestone Member and Donghe sandstone interval of Carboniferous are the main sections for petroleum exploration.
论文运用层序地层学、现代沉积学及储层地质学等新理论,以岩心、测井、钻井、露头剖面测试分析资料及相关基础地质资料为基础,结合前人研究成果,对石炭系生屑灰岩段与东河砂岩段进行了层序地层划分和对比工作,建立了研究区区域等时地层格架,在此基础上,根据钻揭岩性特征、沉积结构和构造特征、测井曲线等指相标志的综合分析,明确了生屑灰岩段主要发育有台地边缘高能生屑滩亚相、局限台地台内生屑滩亚相、局限台地泻湖亚相、局限台地潮坪亚相等主要相带。
3)  Shandong section
山东河段
4)  the eastern section of the Yellow River
黄河东段
1.
After constracting between the Pleistocene ostracods fossil assemblage in the Fenwei Basin and in the Henan Plain district, the author suggests that the eastern section of the Yellow River (east of Sanmenxia) had formed during the initial stage of the Middle Pleistocene or the last stage of the Early Pleistocene, i.
通过汾渭盆地与河南平原地区更新统介形类化石组合的对比,作者认为:黄河东段(三门峡以东)形成的时代为中更新世初期或早更新世末期,里今约七八十万年至一百万年左右。
5)  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
6)  east Suzhou River
苏州河东段
1.
Based on analyzing the historical culture of east Suzhou River,this article did study on this area by four small parts and explained the influences of cultures to the styles of heritage architecture there.
在分析归纳出苏州河东段近代历史文化特征——海派文化和租界文化结合的基础上,分四个区域进行研究,阐释总结了其对两岸优秀历史建筑风格的影响。
补充资料:东河
1.战国秦汉时,黄河自今河南武陟县以下略呈南北流向一段,称东河。与晋陕间北南流向一段称西河相对。 2.清雍正七年(1729年)改河道副总督为河南山东河道总督(通称河东河道总督),专司河南山东两省境内黄河﹑运河等的防治事宜。其所管辖的诸河流统称"东河"。参阅《清史稿·职官志三·总督》。
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