利用岩心分析、测井、地震、薄片分析等静态描述手段测试并计算了基质的孔隙度和渗透率，得到裂缝的宽度、密度和方位等参数。
The porosity and permeability of matrix, and the width, density and direction parameters of fractures were obtained by core analysis, well logging, seism and thin section observation methods.
从岩心薄片分析着手，利用模拟退火算法重建数字岩心；从所建数字岩心中提取对等的由形状简单的孔隙和孔喉组成的孔隙级网络模型。
Based on the analysis of the core slice, simulated anneal algorithm is used to reconstruct digital cores, from which an equal network model made up of pores and throats of simple shape is extracted.
根据微观薄片分析，结合岩心与地表露头资料，对邛西构造须二段特低渗透砂岩储层微观裂缝的类型、特征、期次及其参数分布进行了研究。
The types, characteristics, ages and parameters of the microfractures in T3x2 of Qiongxi structure are studied through microscopic thin section analysis and in combination with core and outcrop data.
在分析这些岩芯时，他们发现冲击石英颗粒———带有特殊排列的微裂缝的薄片，科学家认为他们是外层空间来的物体与地球碰撞留下来的遗迹。
When they analyzed these rocks, they foundshockedquartz grains—slivers with a particular arrangement of micro cracks believed to represent the relic left by an extraterrestrial impact.
取代有代表性的单位厚度的薄片作为分析对象。
A representative slice of unit thickness in then taken for analysis purposes .
分析了复合材料微波检测中电磁参量、电磁波频率和介质薄片厚度的计算方法。
The computation methods of electromagnetism parameters, electromagnetic wave frequency and medium slice thickness in microwave measuring for composite material were analyzed.
综合岩心、薄片、扫描电镜、地球化学等多种分析测试手段，对研究区火山岩岩石类型进行了划分。
The volcanic rock types in the study area have been classified by means of core, thin slice, scanning electron microscopy and geochemical analysis.
本文主要是通过野外的观察和室内岩石薄片的统计分析，来了解尼巴加妖剖面碎屑岩的沉积环境。
On the basis of the field observations and the statistic analysis of thin sections, the author identified the sedimentary environment of clastic rocks from the Nibajiayo section.
薄片光性观察、X射线衍射分析、差热分析和红外光谱分析证实为地开石。
Results of thin section observation, X-ray diffraction pathern, infrared spectrum and different thermal analysis confirm it as a dickite.
方法分析大量铸体薄片以及扫描电镜、压汞、和X -洐射资料。
Methods the data of the casting film, electron microscope scanning, hydrargyrum driving text and X-diffraction were analyzed.
利用地表露头、岩心、薄片和成像测井等资料，对该区裂缝的成因类型、分布特征及其形成序列进行了分析。
Using the data of outcrops, cores, thin sections and image logs, we analyzed the fracture origin types, distribution characteristics and formation sequences.
对利用玻璃纤维网片作为增强基材的薄片切割砂轮强度进行了力学分析，给出了玻纤网片对薄片切割砂轮增强作用的定量计算公式。
This paper presents a mechanical analysis of the cutting grinding wheel strengthened with glassfiber meshes and the formula to calculate the strengthening effect of the glassfiber meshes.
通过对研究区岩性数据、薄片、扫描电镜以及压汞实验资料的统计分析，对储层的物性特征和孔隙结构进行了研究。
A statistic analysis of lithology, thin section, SEM observation and mercury injection data reveals the physical properties and pore structures of the reservoirs in the study area.
石英薄片的红外吸收光谱可以用来研究石英中的气液包裹体井分析其成因。
The infrared spectra of the quartz thin-section may be used to study fluid inclusions in quartz and analyse their genesis.
粒度中值的确定方法较多，包括粒度分析（激光法、筛析法）、薄片粒度分析及应用测井资料计算粒度中值。
There are many means to detenninating median size, including grain size analysis, thin section and log information.
对薄片激光器的热效应进行了分析，从理论上得出了薄片的热焦距表达式。
Thermal effect of thin disk laser is analyzed. Thermal focal length expression is carried out theoretically.
根据岩石铸体薄片和扫描电镜观察资料，分析了吐哈盆地台北凹陷中侏罗统储集层的岩性特征。
Rock properties of Middle Jurassic reservoir in Taibei sag of Tuha basin have been studied by means of the casting thin sections and scanning electron microscope.
对薄片激光器的输出特性进行了分析，设计了相关参数，并在此参数下得出了光束质量、输出功率和转换效率的理论值。
Characteristics of thin disk laser are analyzed. By using some relevant parameters, we obtain numerical values of beam quality, output power and conversion efficiency.
利用岩石薄片和X射线衍射资料，分析了准噶尔盆地腹部地区蒙皂石粘土矿物的不正常转化。
The abnormal transformation of smectite clay minerals in central Junggar Basin is analyzed according to the petrographic thin section and X - ray diffraction data.
利用X衍射全岩分析方法、粘土矿物定量分析方法和薄片鉴定等方法研究了城华地区延8-延1 0储层岩石学特征和孔隙成因类型。
The petrologic characteristic and the pore types of Y8~Y10 reservoir are studied by X ray diffraction method, the quantitative mineral clay analysis method and thin section analysis method.
利用X衍射全岩分析方法、粘土矿物定量分析方法和薄片鉴定等方法研究了城华地区延8 -延1 0储层岩石学特征和孔隙成因类型。
The petrologic characteristic and the pore types of Y8 ~ Y10 reservoir are studied by X ray diffraction method, the quantitative mineral clay analysis method and thin section analysis method.
应用显微薄片鉴定、铸体薄片和扫描电镜等分析化验资料，将其储集空间分为3种类型：原生粒间孔、次生溶蚀孔、微孔隙，并分析了各种成岩作用对储层性能的影响。
Reservoir space is divided into 3 types, that is original intergranular pore, secondary dissolution pore and micro-pore. The influence of different diagenesis on reservoir is analysed.
本文在详细的光、薄片鉴定和电子探针分析的基础上，首次对其矿石矿物进行了系统的研究。
Its ore minerals were systematically studied on the basis of thin section and polished section microscope observation and EPMA.
文摘：根据岩石铸体薄片和扫描电镜观察资料，分析了吐哈盆地台北凹陷中侏罗统储集层的岩性特征。
Abstract: Rock properties of Middle Jurassic reservoir in Taibei sag of Tuha basin have been studied by means of the casting thin sections and scanning electron microscope.
文摘：根据岩石铸体薄片和扫描电镜观察资料，分析了吐哈盆地台北凹陷中侏罗统储集层的岩性特征。
Abstract: Rock properties of Middle Jurassic reservoir in Taibei sag of Tuha basin have been studied by means of the casting thin sections and scanning electron microscope.
应用推荐