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1)  Serosa-Involved
浆膜受侵
2)  mud invasion
泥浆侵入
1.
Methods of Formation Resistivity Correction for Salty Mud Invasion;
盐水泥浆侵入地层电阻率的校正方法研究
2.
Under mud invasion,resistivities of oil layer and water layer in different radial depth are influenced by various factors.
泥浆侵入条件下,油、水层不同径向深度处电阻率变化所受的影响因素不同,以阿尔奇公式为基础,利用阵列感应测井资料,确定纯水层中水的径向电阻率,计算其它地层中不同径向深度的含水饱和度系数,直观反映地层流体含量的变化,正确识别储层流体。
3.
Based on analyzing main factor of generating low-resistivity hydrocarbon reservoir, the corresponding recognition methods are established respectively according to high bound water saturation, sand shale interlayer deposition and mud invasion as the leading causes of generating low-resistivity hydrocarbon reservoir, and the succes.
通过分析形成低阻油气层的主导因素,按高束缚水饱和度、砂泥间互沉积以及泥浆侵入为主导成因的低阻油气层,分别建立了相应的识别方法,大大提高了低阻油气层识别的成功率。
3)  magma intrusion
岩浆侵入
1.
Influence of magma intrusion on reservoir features of surrounding mud rocks in rift basin-case study of gabbros in Chunxi area of Dongying Sag;
裂谷盆地岩浆侵入对泥质围岩储集性能的影响——以东营凹陷纯西地区辉长岩为例
2.
Preservation conditions of the coalbed methane in Tiefa mining area is systematically studied based on analyses of the lithology and sealing capability of the adjacent rocks of coal bed, later reformation, hydrogeologic conditions, and magma intrusion.
通过对铁法矿区煤层顶底板岩性及其封闭性能、后期改造、水文地质条件及岩浆侵入等几方面的分析,系统探讨了铁法矿区煤层气的保存条件。
3.
The influences of Magma intrusion activity on the clastic rocks include the magma upwarp activity, the baked activity and the hydrothermal activity.
在基性岩浆侵入或喷溢活动中,岩浆中的Fe2+、Mg2+,有利于周围碎屑岩中的蒙脱石向绿泥石转化。
4)  the magma corroding
岩浆侵蚀
5)  Magma underplating
岩浆底侵
6)  Magma emplacement
岩浆侵位
1.
The paper synthesizes domestic and foreign references,suggests three types of magma emplacement according to depth of magma emplacement,distance of magma migration,degree of magma crystallization and advancing their combination types,reviews the process and characteristic of magma emplacement of every emplacement type and discusses magma emplacement space and factors affecting magma emplacement.
岩浆侵位机制是研究地球动力作用的重要依据,综合国内外资料,对岩浆侵位机制提出了按侵位深度、岩浆迁移距离、岩浆结晶程度的分类方案及其联合侵位类型。
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1.侵犯干预。
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