泥质的

Water is easily preserved in the pores and forms the undercompaction of the mudstone layer .

泥质岩层中的孔隙水在向外排运的过程中遵循低速非达西流动规律。

And the pelite schist is the main rock type, and contains the classic medium pressure metamorphic minerals.

泥质片岩是工作区内分布最多的岩石组合，出现了典型中压类型的标型矿物及矿物组合。

Because slack has changed the underground water condition which led to the gathering of underground water at the mudstone cleavage zone, and has decreased the resistance, of which the synthetic 〓 is about 13°, it has made the rock mass about the cleavage slide slsde in the western direction.

从边坡岩体地质力学调查分析、岩体结构分析和采煤对滑坡的影响分析，得出滑坡形成的机理，采煤使P〓岩层中沿NW10°~20°/W15°劈理带贯通而移动，由于松弛改变了地下水条件，使地下水向之集中，该泥质劈理带在过水下摩阻力降低，其综合φ为13°左右，使上覆岩体沿之向西滑动。

Because starting resistance is the characteristic of mud-stone, there is the ultra-pressure of fluid in the pores is inevitable if there are neither cracks nor faults.

因为启动阻力是泥质岩层的固有特征，所以，在没有裂缝或断层的情况下，孔隙流体超压就必然存在。

The yellowish bands are slightly calcareous, while the darker grey bands are more pelitic.

黄带的稍微钙质，而暗灰色带更多的泥质。

A comparison between shaly sand conductivities calculated with the old or new formula and experimental data shows that the new formula is more accurate than old one.

用新、旧公式计算的泥质砂岩电导率与实验数据的对比表明新公式更为准确，建议在测井解释中应用。

The membrane potential of oil-bearing shaly sand is the key to evaluate reservoir with the spontaneous potential log .

在此基础上，通过泥浆电阻率的合理选取，可以增强自然电位测井资料对泥质砂岩储层含油性的定性识别能力。

The longer treatment time of samples would result in the more reduction of compressive strength and Young's modulus,because the shale or clay in rock sample would get soft by the drilling fluid filling.

岩石矿物中的泥质黏土矿物遇到钻井滤液后产生软化效应，致使岩样呈现：经钻井液处理时间越长，其抗压强度和弹性模量下降越多的趋势。

Hydrocarbon source rocks are distributed in craton basins and in-tracratonic rift basins.

碳酸盐岩是主要的储集层，泥质岩是主要的区域和局部盖层。

Comparing the data which before the correction and after the correction, we can estimate the actual correction effection of the porosity, permeability and saturation of water, and calculate many important interpretation parameters such as saturation of bound water, mid-value of granularity and content of mud.

通过层厚校正前后的测井数据来评价孔隙度、渗透率以及含油水饱和度等地质参数，并进行束缚水饱和度、粒度中值和泥质含量等各种解释参数的定量计算。

Plunder melds and run with this jewel!

掠夺melds和运行与此宝石！

My dream is to be a crazy growing tree and extend at the edge between the city and the forest.

此刻，也许正是在通往天国的路上，我体验着这白色的晕旋。