| 1. | Design and making of synthetic cores for laminated and dispersed shaly sands
混合泥质砂岩人造岩心的设计和制作 |
| 2. | Establishment of dual water conductivity model for laminated and dispersed shaly sands
混合泥质砂岩双水电导率模型 |
| 3. | Experimental measurement of synthetic core samples for laminated and dispersed shaly sands
混合泥质砂岩人造岩样的实验测量 |
| 4. | The thesis includes two parts basically , and one model was established in each part for studying permeability of shaly sandstones
对于泥质砂岩渗透率的研究，全文共分为两大部分，建立了两个预测渗透率的模型。 |
| 5. | The experiment results show that conductance of laminated and dispersed shaly sands may be treated as parallel conductance between laminated shale and dispersed shaly sands
实验结果表明，混合泥质砂岩导电可以看作是层状泥质和分散泥质砂岩并联导电的结果。 |
| 6. | In the first part , it was discussed that the effect of different distribution of shale in shaly sandstones on their permeability based on capillary buddle model
第一部分，在毛细管束模型基础上，从流体力学理论出发，探讨了泥质的不同分布形式对渗透率的影响。 |
| 7. | In order to reveal the conductance laws of laminated and dispersed shaly sands , conductivity of synthetic core samples with different salinities and different water saturations is measured
摘要为揭示混合泥质砂岩的导电规律，测量了不同矿化度和不同含油饱和度的岩样电导率。 |
| 8. | And the shaly sandstone is the primary type of hydrocarbon reservoirs now . so it is the completely necessary and very significative task to study permeability of shaly sandstone reservoirs
并且泥质砂岩储层是当今石油的主要储集岩石的类型，因此研究泥质砂岩储集层的渗透率是十分必要而且非常有意义的工作。 |
| 9. | Abstract : overpressure was thought to be existed in the shallow layer of songliao basin because several - hundred - meter - think regional shaly rock distributes steadily in qingshankou formation , nen and nen members
文摘:松辽盆地浅层被认为是存在超压的，因为青山口组和嫩一、二段地层稳定分布着几百米厚的区域性泥质岩层。 |
| 10. | Although there is not steadily distributed thicker shaly rock in the deep part of songliao basin , we believe that the deep part is better than shallower part when considering the geologic conditions of forming abnormal pressure
松辽盆地深层虽然没有稳定分布的较厚泥岩层，但从形成压力异常的地质条件看，深层要优于浅层。 |
