| 1. | Origin and sedimentary sequence of es3 - es2 in shahejie formation of dongying depression
二段下亚段沉积层序及成因 |
| 2. | Stratigraphic classification and correlation in es3 of jiuzhou - gu an tectonic belt
固安构造带沙三段地层划分与对比 |
| 3. | The sediment of es3 and es4 member and prediction of favorable reservoir in the wendong - qianliyuan area , dongpu depression
沙四段沉积特征和有利储集体预测 |
| 4. | Study on sedimentary simulation of fan delta in lower sub - member es3 of baimiao gas field in puyang depression
濮阳凹陷白庙气田沙河街组三段下亚段扇三角洲沉积模拟研究 |
| 5. | Analysis on sedimentary system and research on reservoir - forming regularities of es3 in the east part of south slope , dongying sag
东营凹陷南坡东段沙三段沉积体系分析及油气成藏规律研究 |
| 6. | Glutenite sedimentary characteristics analysis taleogene period of es3 4 fan delta in wangzhuang area of dongying depression
东营凹陷王庄地区古近纪沙河街组三段扇三角洲砂砾岩体沉积特征分析 |
| 7. | Oil - source correlation analysis has shown that the oils were mostly from ed2 source rocks from the bozhong depression , and the oils occurred in the slope hidden hill belt were from es3 or / and es , source rocks in the bozhong depression
油源对比结果表明东斜坡带东营组原油来源于渤中凹陷ed _ 2暗色泥岩，斜坡潜山带原油来源于渤中凹陷es _ 3或es _ 1生油岩。 |
| 8. | 4 . based on the research of geochemical characters of hydrocarbon source rock and comparison of oil and gas sources , it is indicated that the condensed oil and gas in buried hills mainly came from es3 effective hydrocarbon source rock of type iii kerogen - type ii2 kerogen in banqiao deprssion and qikou depression beside both sides of the tilting horst , and which is the main source of buried hill with early reservoir and late oil and gas source
4根据烃源岩地球化学特征和油气源对比，指出潜山凝析油气主要来自翘倾地垒块两侧板桥和歧口凹陷的沙三段腐植-偏腐植型有效烃源岩，该凝析油气是“新生古储”型潜山的主要油气源。 |
| 9. | The biomarker characteristics of these two types of viscous oils are distinctive . oil source correlation results show the altered viscous oils were generated from the es3 source rocks and subsequently suffered biodegradation , oxidation and water washing effects near the surface . there exists huge thick alluvial glutinite in luojia - kenxi area , with various physical properties
两类稠油生物标志物组成也有明显的差异，次生稠油主要由来源于沙三段源岩的正常原油(稀油)经生物降解、地表氧化、水洗等次生作用形成的，并且成熟度指标相对较高。 |
| 10. | Futhermore , the formation of reservoir experienced four periods : the first , from esi to ed ; the second , from late ng to early nm ; the third , nm ; the fourth , from late nm to now . so we predict that exploration in qianmiqiao should be mainly directed to condensed oil and gas reservoir nearby banqiao depression and gas reservoir is more probably found near qikou depression . 8 . analogue of the conditions required for reservoir formation in huanghua buried hills shows that , high quality and thick es3 hydrocarbon source rock distributed richly in the middle area depression , and moderate quality sandstone distributed in south area , but the match bet
8对黄骅坳陷区“新生古储”型潜山成藏条件的类比分析表明，中区凹陷中分布有厚度较大的优质沙三段烃源岩，南区分布有较好的孔二段烃源岩，但中区千米桥地区生储配置比南区好，因此，整体上中区千米桥潜山一带油气藏的勘探前景优于南区。 |
