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.
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
4.
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
5.
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
6.
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
7.
Prediction of the Secondary Porosity Zone of Fuyu Oil Layer in the West of Daqing Placanticline
大庆长垣以西地区扶余油层次生孔隙预测
8.
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。
9.
Materials having induced porosity such as the carbonate rocks have even more complex pore configurations.
类似碳酸盐岩这种含有次生孔隙结构的物质具有更为复杂的孔隙构型。
10.
Diagenesis and Secondary Pore Feature of Sandstones of the Sub-member S_3~2 of the Eogene Shahejie Formation in the Baimiao Area of the Dongpu Depression
东濮凹陷白庙地区沙三~2亚段砂岩成岩作用及次生孔隙特征
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.
MECHANISM OF FORMATION FOR SECONDARY POROSITY OF CRETACEOUS RICH FELDSPAR SANDSTONE IN SONGLIAO BASIN AND ITS CONTROL FACTORS
松辽盆地白垩系富长石砂岩中次生孔隙形成机制与控制因素
14.
Study of Petrological Characteristics and Thermodynamic Mechanism of Secondary Pores in Deep Reservoirs, Songliao Basin;
松辽盆地深层储层岩石学特征及次生孔隙形成热力学机制
15.
Distribution and Origin of Secondary Pores in Xujiahe Formation Sandstone Reservoirs in Mid-south Sichuan Basin
川中—川南过渡带须家河组砂岩储层次生孔隙成因与分布特征
16.
For the Characteristic of the Dissolution of Primary Minerals Related to Clastic Diagenesis Thermodynamics Model and Dissolution Experiment Modeling Effort for Secondary Porosity Forming Mechanisim of Upper-Palaeozoic, Qrdos Basin;
鄂尔多斯盆地上古生界碎屑岩次生孔隙形成机制的热力学计算和溶解实验模拟研究
17.
Induced porosity is typified by fracture development as found in some shales and limestones and by the vugs or solution cavities commonly found in limestones.
次生孔隙度是以某页岩和石灰岩的裂缝和石灰岩中的岩穴和溶洞为代表。
18.
Three high carbonate belts and four secondary pore belts developed vertically in the reservoir rocks of the Eogene Shahejie Formation in Dongpu Depression.
东濮凹陷下第三系沙河街组储层在纵向上有三个高碳酸盐含量带和4个次生孔隙发育带。