| 1. | Ideas on the petroleum geology conditions of yanji basin
对焉耆盆地油气地质条件的认识 |
| 2. | The time in yanqi
焉耆的时间 |
| 3. | Relations between jurassic inclusions and oil amp; gas migration amp; accumulation in yanqi basin
焉耆盆地侏罗系包裹体与油气运聚期次的关系 |
| 4. | Yanqi basin , located in the northern wing of the " v - type " thrust - fold belt , is related to the reversion of the kuluketage aulacogen
因此库鲁克塔格裂陷槽的构造反转是焉耆盆地构造变形的主要力学来源。 2 、描述了盆地内的构造样式。 |
| 5. | Yanqi basin is a typical reformed residual basin where several oil and gas fields with commercial value and some product energy have been found in recent years
焉耆盆地是一典型的改造残留盆地，在其中已发现多个有商业价值和一定规模产能的油气田。 |
| 6. | Interpreting the remote sensing images and verifying the facts in south tian shan , we studied active tectonics of yanqi basin , aheqi fault and kuche depression
通过遥感图像和野外实际验证相结合的研究方法，对南天山焉耆盆地、阿合奇断裂和库车坳陷的活动构造进行了研究。 |
| 7. | Yanqi basin is stituated between tarim basin and tarpan - harmi basin . its petrolenm system underwent the formation and destruction during jurassic - cretaceous , the activation and reconstruction during tertiary - quaternary
焉耆盆地位于塔里木盆地和吐哈盆地之间，其含油气系统经历了侏罗纪-白垩纪的形成与破坏阶段和第三纪-第四纪的活化与再建阶段。 |
| 8. | Aiming at the abnormal phenomenon that water content of some production wells with decline along with the time in the yanqi basin , this paper puts forward an argument that low water - cut oil layers exist in the low permeability formation
摘要针对焉耆盆地部分生产井，在投产过程中存在随时间的延长含水率下降的反常现象，提出了低渗地层存在低含水油层的观点。 |
| 9. | The tectonic framework and border faults of the basin were related to the basement configuration . 3 . based on the regional tectonic setting and sedimentary sequence evolution , the structural physics modeling and balance profile reversion are first carried out
焉耆盆地前中生代基底硬块的形态及内部结构对中新生代盆地的形成及形变具有重要的控制作用，现今盆地的构造格局和重要的边界断层都与基底的结构有关。 |
| 10. | Yanqi basin is an intermont basin of tian shan , there is a nww trending right lateral strike slip active fault in southwestern basin , its maximum slip distance is 210m , and slip rate is about 10mm / yr , moreover , there is a west - east trending active anticline along northern basin
焉耆盆地是一个天山山间盆地，盆地西南缘发育一条走向北西西的右行走滑活动断层，最大走滑距离为210m ，走滑速率约10mm / yr ，盆地西北缘发育走向近东西的活动褶皱。 |
