1) secondary minerals
次生矿物
1.
Precipitation of secondary minerals is crucial to groundwater evolution and radionuclide retardation in water-rock systems.
水-岩反应次生矿物的沉淀作用不仅控制着地下水成分的演化,而且对核素的迁移和阻滞作用有重要影响。
2) primary and secondary minerals
原生和次生矿物
3) secondary
次生
1.
A study of the secondary dissolution pores in the volcanic reservoirs of Xingcheng development area can provide a basis for future exploration and development of the Xushen gas field.
对徐深气田兴城开发区火山岩储层次生溶蚀孔隙进行研究,可为今后该气田的勘探开发工作提供依据。
2.
However, these rigid and dense carbonates and thick-bedded sandstones are of relatively developed secondary fractures (fissures) and solutional pores, which are mainly distributed in four suites of rigid rocks.
然而对于刚性致密的碳酸盐岩以及厚层块状砂岩,次生裂隙(缝)、溶隙相对发育,它们分布于四套主要的刚性岩层中,极大地改善了这些岩石的孔渗性能,使之成为良好的裂隙储集体,为海相中生界、古生界油气聚集成藏提供了有利的储集空间。
4) secondary hydrocarbon generation
二次生烃
1.
Control role of primary hydrocarbon temperature-increasing velocity of organic matter to the secondary hydrocarbon generation;
有机质初次生烃升温速率对二次生烃的控制作用
2.
Discussion on hydrocarbon generation potential and secondary hydrocarbon generation of organic matter from Permo-Carboniferous coal measures in the southern North China;
南华北地区石炭-二叠纪煤系生烃潜力与二次生烃探讨
3.
Researches on secondary hydrocarbon generation in Southwest of Jianghan Basin and its effects on hydrocarbon accumulations;
江汉盆地西南缘二次生烃及其对油气成藏的影响
5) secondary pores
次生孔隙
1.
Effectiveness of thermochemical sulfate reduction on oil and gas industry—a H_2S formation accelerating development of the secondary pores in reservoirs;
TSR(H_2S)对石油天然气工业的积极性研究——H_2S的形成过程促进储层次生孔隙的发育
2.
Distribution and genesis of secondary pores in Tertiary clastic reservoir in Southwestern Qaidam Basin;
柴西南地区第三系碎屑岩储集层次生孔隙分布及成因
3.
Genesis of heterogeneity of secondary pores in deep reservoir of Jiangling Depression;
江陵凹陷深层储层次生孔隙非均质性成因
6) secondary pools
次生气藏
1.
The Shaximiao Formation gas reservoirs in Luodai gas field are secondary pools,which locat.
在好的沉积微相中,优质储集砂体的发育,建设性成岩作用对储层物性的改善,向上跨层断层及裂缝系统的不发育,都是沙溪庙组"过路型"次生气藏高产气井的主控因素。
参考词条
补充资料：次生铀矿物
分子式：
CAS号：
性质：原生铀矿物受到外界条件作用(如风化作用、变质作用和溶蚀作用)后，改变其结构和成分重新生成一种具放射性的矿物。如沥青铀矿变成铀黑和硅钙铀矿等。
CAS号：
性质：原生铀矿物受到外界条件作用(如风化作用、变质作用和溶蚀作用)后，改变其结构和成分重新生成一种具放射性的矿物。如沥青铀矿变成铀黑和硅钙铀矿等。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。