1.
secondary porosity index log
次生孔隙度指数测井
2.
Porosity may be classified according to the mode of origins (1) original and (2) induced.
按其原始形态，孔隙度可分为原生孔隙度和次生孔隙度。
3.
FRACTAL DIMENSION ACHIEVES FRACTURED ROCK POROSITY INDEX M AND ITS APPLICATION
分形分维求取裂缝性岩石孔隙度指数m及应用
4.
formation facctor-porosity relationship
地层因数-孔隙度关系
5.
decimal porosity
以小数表示的孔隙度
6.
The pore spaces are completely dominated by primary porosity and pores, vogs and fractures with secondary origination.
孔隙空间主要是原生孔隙及由次生原因形成的孔隙和裂缝。
7.
ocks having original porosity are more uniform in their characteristics than those rocks in which a large part of the porosity is induced.
具有原生孔隙度的岩石比次生孔隙度占大部分的岩石在性质上更具有一致性。
8.
Comparative Study on Predicting Porosity by Different Roughness Indices
不同粗糙度尺度下预测表层土壤孔隙率量化指数比较研究
9.
Stress sensitivity has relationship with water saturation of reservoirs.
低渗透气藏岩心的孔隙度随有效压力的增大呈指数关系递减。
10.
Influence of Sandstone Pore Texture on Cementation Exponent and Saturation Error Analysis in Kuche Area,Tarim Basin
库车地区砂岩孔隙结构对胶结指数影响及饱和度误差分析
11.
The diagenetic environment results in different water-rock reaction and development of secondary porosity.
成岩环境在一定程度上影响了水岩反应及次生孔隙发育。
12.
RELATIONSHIP BETWEEN TEMPERATURE-PRESSURE AND SECONDARY PORES OF DEEP RESERVOIRS IN EOGENE AT JIYANG DEPRESSION
济阳坳陷下第三系温度、压力与深部储层次生孔隙的关系
13.
porosity-compressibility product
孔隙度-综合压缩系数乘积
14.
Original porosity is typified by the intergranular porosity of sandstones and the intercrystalline and politic porosity of some limestones.
原生孔隙度以砂岩粒间孔隙度和某些石灰石的晶体粒间和鲕状孔隙度为代表。
15.
The Development Mechanism of the Secondary Pores in the Reservoirs of the Down-Faulted Basins of the Late Mesozoic Era in the Northeast of China
东北晚中生代断陷盆地储层次生孔隙形成机制
16.
The Developing Regularities and the Developing Zones Forcasting of Secondary Pore of Fu-Yu Reservoir in Qijiabei Area, Songliao Basin;
松辽盆地齐家北地区扶余油层次生孔隙发育规律及次生孔隙发育带预测
17.
Fundamental characteristics and itscontrol factorsover secondary pores of Eogene system sandstone in Jiyang depression
济阳拗陷砂岩次生孔隙的基本特征及控制因素
18.
DISTINGUISHING VOLCANIC ROCK RESERVOIRS WITH T2 SPECTRA OF NUCLEAR MAGNETIC RESONANCE(NMR)
应用核磁共振T_2谱划分火成岩次生孔隙储层