1) the north slope of Fuxin uplift zone
扶新隆起带北坡
2) Fuxin uplift belt
扶新隆起带
1.
Xinmiaoxi area is situated in the north slope of Fuxin uplift belt,south Songliao basin,where the main reservoirs are characteristic of thin and interbedded sandstone/mudstone that belong to outer frontal sedimentary facies of delta.
新庙西地区位于松辽盆地南部扶新隆起带北坡,主要储层为砂泥岩薄互层,属三角洲外前缘沉积相带,储层横向变化快,砂泥岩薄互层中砂、泥岩速度差别小,波阻抗反演不能有效地识别砂岩,因此预测砂泥岩薄互层储层难度较大。
3) Fuxin uplift
扶新隆起
1.
Inclusion analysis indicates that Fuxin uplift and Changling sag separate away after major reservoir-forming stage of Fuyu oil layer, i.
包裹体分析结果表明,吉林油田扶新隆起和长岭凹陷是在青一段生烃高峰后和扶余油层主成藏期后才发生明显的“隆—凹”分异,即油气充注和成藏发生于扶新隆起大规模隆升之前。
4) Jiaobei uplift belt
胶北隆起带
1.
Low greenschist factes(epizonal) regional metamorphism in the Ponglai Group has been determined in this paper by measurement of illite crystallinity values of the Ponglai slates in the Jiaobei uplift belt,eastern Shandong.
本文应用鲁东胶北隆起带上蓬莱群板岩中伊利石结晶度值测量，确定了蓬莱群经历过低绿片岩相（浅变带）区域变质。
5) south and north slope of protrusion
隆起南北斜坡
6) The North Slope of Chengning Uplift
埕宁隆起北坡
1.
The north slope of Chengning uplift is one region which has huge prospect potential in Huanghua depression in Neogene.
埕宁隆起北坡是黄骅坳陷新近系具有较大勘探潜力的地区，研究其沉积与层序特征对于油气勘探和开发有重要的现实意义。
补充资料：扶扶
1.幼小貌。汉扬雄《太玄．礥》:"赤子扶扶，元贞有终。测曰:赤子扶扶，父母詹也。"范望注:"扶扶幼小之貌也。"一说，依慕之意。司马光集注:"扶扶，扳援依慕之意。"
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参考词条