1) Wenliu area
文留地区
1.
The hydrocarbons in Dongying Formation reservoir in Wenliu area,the Dongpu Sag of the Bohai Bay Basin,have undergone various degrees of biodegradation as the results of being relatively shallowly buried.
渤海湾盆地东濮凹陷文留地区东营组埋藏较浅,储层中的烃类受到不同程度的生物降解。
2.
The gas in Es3(4) below the salt sequence has single source in Wenliu area of Dongpu depression, and the boundary condition is clear for the source rocks in the CarboniferousPermian coalbearing sequence.
东濮凹陷文留地区沙三段4亚段盐下气源单一,石炭—二叠纪系煤系气源边界条件清楚,该区勘探程度高,对天然气成藏条件、成藏历史、气藏特征的认识深刻,可以有依据地推算最终可探明储量;利用盆地模拟方法计算出刻度区的煤系生气量,进而推算出天然气聚集系数为7。
3.
Group composition and carbon isotope of oil,chromatogram and mass spectrum of aliphatic are analyzed from samples source rock,crude oil and oil sand in Wenliu area Dongpu depression.
运用地球化学研究手段,对东濮凹陷文留地区原油、油砂和泥岩进行了族组分、碳同位素和饱和烃色谱-质谱分析,文留地区沙三段原油族组分含量表现为高饱和烃、芳烃与低非烃和沥青质;原油族组分碳同位素具有海相有机质的碳同位素组成特征,反映有机质生物源主要来自盐湖相的水生生物和细菌;植烷优势明显,甾烷参数C29αα20S/(20S+20R)为0。
2) Wenliu region
文留地区
1.
Reservoir forming of the fractured mudstone reservoir with salt interbed in Wenliu region;
文留地区盐间泥岩裂缝油气藏成藏作用
2.
This paper is focus of the theory of paleogene salt rock sedimentation in the Wenliu region,analyses the relation between the salt rock and oil-gas gathering.
为了探讨文留地区盐岩的形成机理 ,分析盐岩与油气的聚集关系 ,归纳总结了文留地区下第三系沙河街组盐岩分布特征 ,利用古生物种群演化和构造发育史理论 ,对文留地区盐岩进行深入细致的研究 ,结果给出了本区成盐模式的合理解释及其与油气聚集的关系。
3) Liuxi Area
留西地区
1.
Sedimentary facies and subtle petroleum reservoirs of the upper submember of Member 3 of Paleogene Shahejie Formation in Liuxi area of Raoyang Sag,Jizhong Depression;
冀中坳陷饶阳凹陷留西地区古近系沙河街组沙三上亚段沉积相与隐蔽油藏
2.
Sequence stratigraphy of the upper third member of the Shahejie Formation in Liuxi area of the Raoyang Sag,the Jizhong Depression and exploration of subtle reservoirs
冀中坳陷饶阳凹陷留西地区沙三上亚段层序地层与隐蔽油藏
3.
The conditions for oil accumulation is Liuxi Area of Raoyang Depression are analyzed.
分析了饶阳凹陷留西地区的成藏条件。
4) Wenliu graben
文留地堑
5) message retention area
报文存留区
6) Wendong area
文东地区
1.
The study suggests that the sedimentary facies and sand body types of the middle sub-section of the Es~3 in the Wendong area,Dongpu Sag,are developed neither in shallow water nor in deep water,it should be a sediment developed in the alternate environments between shallow and deep water.
对东濮凹陷文东地区沙三中亚段的研究表明,其沉积环境不能简单地认为是深水的或浅水的,而是深水和浅水环境交替出现。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
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