1.
Mechanism of Carbonate Cementation and Secondary Dissolution Porosity Formation in Deep-Burial Sandstones near the Top Overpressured Surface in Central Part of Junggar Basin
准噶尔盆地腹部超压顶面附近深层砂岩碳酸盐胶结作用和次生溶蚀孔隙形成机理
2.
secondary porosity index log
次生孔隙度指数测井
3.
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。
4.
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。
5.
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
6.
Character and Comparison of the Carbonate Dissolved-Porosity Reservoirs of the Jialingjiang Formation in Miaogaosi-Erlichang Area
庙高寺-二里场嘉陵江组溶蚀孔隙型储层特征分析
7.
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。
8.
The karst fissure medium can be regarded as dual medium of porosity.
岩溶裂隙介质可视为双重孔隙度介质。
9.
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
10.
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
11.
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
12.
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
13.
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
14.
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。
15.
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。
16.
THE EVOLUTION OF THE POROSITY AND THE SECONDARY PORE SPACE IN NO.Ⅶ RESERVOIR SANDSTONES,SHUANGHE OIL FIELD
双河油田Ⅶ油组砂岩的孔隙演化和次生储集空间
17.
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
18.
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。