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1)  perforation types
孔眼类型
2)  porosity type
孔隙类型
1.
On the basis of micro section identification data of the reservoirs, the author considers that the main factors affecting physical property parameters are rock type, grain size, porosity type and clay content.
根据岩石薄片鉴定资料分析 ,影响物性参数的因素有 :岩石类型、粒度大小、孔隙类型、泥质含量。
3)  Pore types
孔隙类型
1.
These characteristics include petrofabric,diagenesis types,pore types,distribution rules of clay and diagenetic stage.
本文以岩矿测试分析与镜下鉴定等资料为依据,详细地研究了柴达木盆地北缘冷湖地区下侏罗统碎屑岩储集层的岩石学特征、成岩作用类型、孔隙类型、粘土矿物分布特征、成岩作用阶段等特征。
2.
This paper,based on many more analytical data,describes the petrophysical properties,pore types and pore textures of deep reservoirs,and divides three types of reservoirs,such as low permeability,medium permeability,and tight reservoirs,of which the low permeability reservoirs are widely spread,and the medium permeability reservoirs are hug.
在进行了大量的分析化验基础上 ,研究了深部砂岩储集层的物性、孔隙类型和孔隙结构特征 ,划分出低渗型、致密型和中渗型 3种类型储集层 ,其中低渗型分布最广 ,中渗型油气勘探潜力巨大。
3.
Based on the pore types of carbonate core in Carboniferous in East Sichuan, combining the logging curve characters of the various pore types, a method for discriminating the pore types of the carbonate reservoir is carried out, which is help to raise logging coincidence rate of quanlitatively discriminating gas and water layeres and quantitatively interpreting the accuracy.
本文以川东石炭系碳酸盐岩岩心孔隙类型为基础,结合各种孔隙类型的测井曲线特征,研究得出了判别川东石炭系碳酸盐岩储集层孔隙类型的方法。
4)  pore type
孔隙类型
1.
Analyzing well log,well testing,and the core data,this paper discovered that the difference among pore types in the reservoirs is the main reason that the different logging response characteristics existed in the fluid with the same properties,and the misjudgement occurred mainly in the intercrystal p.
研究中对实钻井的测井、试油和岩心分析资料进行对比分析,最终认识到储层孔隙类型的差别是影响储层含流体性质的测井特征响应不同的主要原因,误判层主要发生在以晶间孔为主的储层。
2.
Based on the data of lithologic analysis and microscopic examination,the characteristics are studied,which include lithology,diagenesis type, pore type,clay mineral distribution and stage of diagenesis of clastic reservoirs in Lower Jurassic on the north margin of Lenghu area in Qaidam Basin.
以岩矿测试分析与镜下鉴定等资料为依据,详细地研究了柴达木盆地北缘冷湖地区下侏罗统碎屑岩储集层的岩石学特征、成岩作用类型、孔隙类型、粘土矿物分布特征、成岩作用阶段等特征。
3.
It is concluded that these clastic reservoirs have low compositional and textural maturity, diagenesis is the early deep-burial later elevating type, pore types are constituted of residual intergranular pores, small amount of dissolution intergranular pores, ma.
在微观研究的基础上,对储集层沉积埋藏史、岩石学特征、孔隙结构、成岩作用以及孔隙演化特征等进行系统分析,认为哈密坳陷三叠系至下侏罗统碎屑岩储集层成分和结构成熟度低,成岩作用属早期深埋晚期抬升型,孔隙类型组合是以残余粒间孔-少量溶蚀粒间孔-大量微孔隙-成岩缝为主的组合,孔隙结构差,成岩阶段大部分已进入晚成岩B亚期。
5)  types of fracture
孔缝类型
6)  keyhole mode
穿孔类型
补充资料:血液有形成分各种类型的血细胞虚线指示中间类型的细胞。




血液有形成分  各种类型的血细胞  虚线指示中间类型的细胞。
                                       李瑞端绘
  [图]图

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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