1.
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
2.
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
3.
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
4.
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
5.
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。
6.
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。
7.
secondary porosity index log
次生孔隙度指数测井
8.
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
9.
Secondary interstices develop after the rock is formed.
在岩石形成以后再发展次生间隙。
10.
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
11.
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
12.
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。
13.
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
14.
The Mechanism of Pore Formation in Superconducting MgB_2 Synthesized at Low Temperature by In-Situ Process
原位法低温合成MgB_2的孔隙形成机制
15.
The configuration of the pore space is different from that which would be obtained from the packing of uniform spheres.
自然界物质孔隙结构与均匀球粒的堆积而形成的孔隙是不同的。
16.
Study indicates that the formation and evolution of the porosity are controlled by diagenesis.
研究表明：孔隙的形成和演化受成岩作用的控制。
17.
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
18.
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