1) fourth member of Yingcheng formation
营城组营四段
1.
Hydrocarbon exploration demonstrated that the sandy conglomerates of the fourth member of Yingcheng formation(FMYF) in Xingcheng gas field of Xujiaweizi fault depression have some potentialities.
天然气勘探证实徐家围子断陷兴城气田营城组营四段砂砾岩具有较好勘探潜力。
4) Ying-4 section
营四段
1.
Study shows that Ying-4 section is a set of conglomerate reservoir with extremely low porosity , permeability and presenting fissure, the average porosity is 3.
通过精细岩心观察、普通薄片、铸体薄片及扫描电镜等资料,对兴城气田营四段砾岩储层的储集空间类型进行了研究。
5) Yingcheng Formation
营城组
1.
Joint Structure Features,Distribution Regularity and Reservoir Prediction of Yingcheng Formation in Eastern Songliao Basin;
松辽盆地东缘营城组节理构造特征、分布规律及其储层预测
2.
Sedimentary Characteristics and Origin Model of Conglomerate of Second Member,Yingcheng Formation in Liutai,Southeast Margin of Songliao Basin;
松辽盆地东南缘六台地区下白垩统营城组二段砾岩沉积特征及成因模型
3.
Types,Characteristics and Genesis of Lithophysa in Rhyolite of Yingcheng Formation,Songliao Basin;
松辽盆地白垩系营城组流纹岩中石泡构造类型、特征及成因
6) the third member of Dongying formation
东营组三段
1.
The Variation Characteristics of Reservoir Plane Heterogeneity in Different Development Stages of Oilfield: Take the third member of Dongying formation in the second block of Shengtuo Oilfield as an example;
油田开发阶段储层平面非均质性变化特征:以胜坨油田二区东营组三段为例
补充资料：金四郎城古城遗城
金四郎城古城遗城位于锡林郭勒盟正蓝旗敦达浩特北两公里处。城址为乌桓游牧故地，故命名为桓州城。始建于金代。古城呈方形，东西长1052.5米，南北宽1136.8米，东西两面城门至今尚可辩认。城墙夯筑不明显，残高3-5米，每隔60左右米有凸出的马面。城中有建筑台基遗迹，为州府官衙所在。古城内散布着大量残砖碎瓦，瓦背为素面反面布纹，砖多是灰色素面，有少量沟纹砖。古城内曾出土过粗瓷双耳罐、铁斧及定窑、钧窑瓷片。
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参考词条