Four hypotheses of secondary pore forming mechanism are introduced.
介绍了次生孔隙成因机制的四种假说。
The reservoir pore evolution changed from primary to secondary pores.
储层孔隙经历了由原生到次生的演化过程。
On the basis of studying secondary pore, the direction of next exploration is predicted.
在次生孔隙研究基础上，预测了下一步勘探方向。
Reservoir species are mainly residual inter-granular pore-space and inner-granular corrosion secondary pore-space.
储层中残余原生粒间孔保留程度是决定储层质量的关键因素。
Exploration results have proved that newly found reservoirs are largely distributed in the laumontite secondary pore zone.
勘探结果证实延长统找到的油藏大部分都聚集在这些浊沸石次生孔隙中。
The pore types include primary intergranular pores and secondary pores, with the latter being mainly of intergranular dissolved pores.
孔隙类型包括原生粒间孔和次生孔隙，后者以粒间溶孔为主。
The porosity increasing is primarily due to the resolution of carbonate so that a large amount of the secondary pore space is resulted.
而碳酸盐的溶解作用形成了大量次生孔隙空间，增加了砂岩的孔隙度。
To some extent, the chemical erosion made the physical property of reservoir getting better and increased the secondary pore relatively.
而溶蚀作用从一定程度上使储层物性得到了改善，次生孔隙相对增多。
The early diagenesis mainly influences the development of primary pore and the late diagenesis mainly influences the development of secondary pores.
早期成岩作用主要影响原生孔隙的发育，晚期成岩作用影响次生孔隙的发育。
As the main flow manner of formation water in deep reservoir, circulated convection current controlled authigenic mineral location and secondary pore distribution.
循环热对流是深部储层流体的主要流动方式，它控制着自生矿物在砂层中的析出位置和次生孔隙的分布特征。
The Y-type zeolite with optimized secondary pore structure has an relative XRD crystallinity over 70 % and a secondary pore volume of 20-80 % by total pore volume.
一种具有优化的二级孔结构的Y型沸石及其制备方法，该沸石的XRD相对结晶度在70%以上，二级孔体积占总孔体积的百分数为20 ~ 80%。
The main pore type of the reservoir is primary remained intergranular pore, the dissolution of the feldspar and early carbonate cement results in the secondary pore.
储层以原生剩余粒间孔隙为主，长石及早期碳酸盐胶结物的溶解是形成次生孔隙的主要原因。
Sedimentary facies zone and diagenesis are major affecting factors for pore reservoir structure. The growth of secondary pore zone is closely related to dissolution.
沉积相带和成岩作用是影响储层物性的主要因素，次生孔隙带的发育与溶蚀作用关系密切。
Generally, different sedimentary microfacies developed different types of cementation that controlled distribution of secondary pore dissolved by acid water solution.
不同的沉积微相其胶结类型不同，从而导致酸性水溶蚀次生孔隙所发育的程度迥异。
Reservoir study shows there have been primary and secondary reserving pores developed in the volcanic rock reservoirs of this area, the secondary pore being dominant.
储层研究表明，本区火山岩储层主要发育原生和次生两种储集空间，以次生储集空间为主。
The compactionand secondary enlargement of quartz lead to the great decrease of primary porosity of clastic rocks, and dissolution is contributed to the formation of secondary pore space.
压实作用和石英的次生加大使碎屑岩的原生孔隙度极大的降低，溶解作用是次生孔隙形成的主要因素。
Using electro-imaging data, the paper uses ELAN program and program of pore spectrum analysis to analyze and study secondary porosity of Budat formulation in Hailar basin.
文中利用电成像测井资料，采用ELAN程序、孔隙频谱分析程序对海拉尔盆地布达特地层的次生孔隙率进行分析研究。
Many vessel numbers, small pore, libriform fibres (mechanical tissue)and obvious secondary thickening of xylem tissue are the features of adaptation to the environment.
红树植物导管数量多、管孔小、机械组织为韧型纤维，薄壁组织次生加厚明显是适应环境的特征。
It is pointed out that reservoir space of conglomerate is composed of primary intergranular pore, hole and fracture, secondary denudation pore and structural fracture.
指出，砾岩的储集空间为原生砾间孔、砾间洞、粒间缝、次生溶蚀孔和构造缝。
The types of the pore are mainly secondary solution pores and seldom primary remanent intergranular pores.
孔隙类型主要为次生溶孔，偶见剩余原生粒间孔。
The reservoir space of oil bearing sandstone is mainly secondary porosity and it's a pore type reservoir and its lateral variation is governed by the depositional and diagenetic process.
油层的储集空间以次生溶蚀孔隙为主，属孔隙型储集类型。储层受沉积、成岩变化控制，引起物性横向变化。
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.
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.
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。
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