研究表明，飞仙关组储层主要受沉积作用和成岩作用的控制。
Study suggests that Feixianguan formation is essentially controlled by sedimentation and diagenesis.
用数学方法模拟计算了泵浦作用时非饱和情形下染料分子的储能和飞秒脉冲的放大。
The store energy of dye molecules and the amplification of fs pulses in condition of under saturable energy were calculated by mathematical simulation.
川东北飞仙关鲕滩储层普遍存在高电阻率现象，给储层识别和流体性质判别带来了很大的困难。
There are many difficulties for judging reservoir and fluid properties because of the Feixianguan Ertan high resistivity zones in the north-east Sichuan.
川东北地区罗家寨飞仙关组鲕滩储集层为碳酸盐岩台地边缘相沉积，具有厚度大、分布稳定的特点。
Oolite beach carbonate reservoir of Feixianguan Formation in Luojiazhai, NW Sichuan Basin is a platform edge facies sediment with massive thickness and uniform distribution.
用岩心流动实验的方法，针对飞仙关鲕滩储层，从暂堵剂的堵塞性及酸化解堵性方面对暂堵剂优选进行了研究。
On the basis of the features of Ertan reservoir in Feixianguan TM, the paper researches the optimum seeking method of temporary plugging agent by using core flow experiment.
综合分析各种因素，才能准确评价川东北飞仙关鲕滩高电阻率储层。
We can exactly evaluate the Feixianguan Ertan high resistivity reservoir by analyzing the factors.
川东地区飞仙关组储层的发育，受有利沉积相带控制。
Development of reservoir in Feixianguan formation of east Sichuan is controlled by favorable sedimentary facies.
应用测井资料识别川东飞仙关组鲕滩储层是个新课题。
It is a new problem to identify the oolitic beach reservoirs of Feixianguan Formation in East Sichuan by log data.
飞仙关组鲕滩储层为裂缝-孔隙型或孔隙型储集类型，储集岩可分为鲕粒灰岩和自云岩，在川东北地区是高产气层。
Oolitic beach reservoir is of fractured or porous reservoirs which include oolitic limestone and dolomite. It is a high gas production reservoir in northern Sichuan province.
四川盆地东北部长兴-飞仙关组是近年来我国发现的重要天然气储集层，已成为我国油气的重点勘探地区之一。
Xing Northeastern Sichuan Basin - Feixianguan is found in China in recent years, an important gas reservoir, has become the focus of China's oil and gas exploration areas.
以往川东地区飞仙关组鲕滩储层预测，主要采用常规剖面寻找“亮点”反射，或作速度反演寻找低速异常体，取得了一定的效果。
The prediction for oolitic reservoirs of Feixianguan Formation was used to looking for bright spots on conventional sections or for low velocity anomalies on velocity data set in east Sichuan.
飞仙关组储集岩为各种颗粒云岩或具颗粒幻影的细粉晶云岩，灰岩类储层欠发育。
The Feixianguan formation's reservoir lithology included all kinds of grain dolostones and fine-crystal dolostones remaining grain apparition exluding the limestones.
通过对川东北长兴-飞仙关组地层沉积相特征的分析，探讨其储层发育的机制。
Through the northeastern Sichuan Changxing - Feixianguan sedimentary facies analysis, reservoir development to explore its mechanism.
通过对川东北长兴-飞仙关组地层沉积相特征的分析，探讨其储层发育的机制。
Through the northeastern Sichuan Changxing - Feixianguan sedimentary facies analysis, reservoir development to explore its mechanism.
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