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The nonlinear phenomena in above experiments can be explained by probability density distribution of micro-cracks.

用岩石样品在恒定压力下的蠕变实验,得到岩石的蠕变曲线。

The result showed that there was an obvious correlation between rock thermal cracking threshold and rock inhomogeneity.

结果表明岩石的热破裂门槛值与岩石非均质度具有显著的相关性。

The mean square error of strength is a measurement of rock mechanics. A new model about relation between strength of rock and its sample size is set up.

研究表明,上述损伤力学模型可以近似地反映岩石的本构性能,强度分布方差是岩石材料物理性能的一种量度。

With the fracture profile method, the dimensions of fractal of the fracture surface of rock was measured.

用侧面轮廓线法测量了岩石断口的分形维数,结果表明,岩石的断裂韧度越大,断口分维数越小。

The mineral component and microstructure of the mudstone are determined.

测定了岩石的矿物成分及微观结构和岩石的物理及水理性质参数。

It lies at the foot of a huge outcrop of rock, upon which is perched the mediaeval city of Orvieto.

它座落在一个巨大裸露的岩石下方,岩石的上方则盘踞了一座中世纪古城Orvieto。

Through the creative research of piezoelectricity of quartz-bearing rocks, the modulus of most kinds of the rocks are given out.

同时还开创性地对含石英岩石的压电性进行了测试研究,得出各类岩石的压电模数值

Acidic rocks have a silica content over 70 % Granite is the typical example of acidic intrusive igneous rock, which is composed mostly of potash feldspar, quartz and minor mica.

岩石中Si02含量大于70%时,称为酸性岩,花岗岩就是酸性侵入岩石的一个典型例子,它的矿物成分主要是钾长石、石英以及少量云母

And the results indicate that the principal stress directions in study area are mainly NE-SW, and the second substage tectonic twist made the direction deflect from North to East, but the primary direction changed little; tectonic activities during the O〓~S~D stage is some violent, most of the area are under high stresses status, and rock fracture degree is correspondingly higher, as coinciding with the drill cores observation, i.

通过数值分析,模拟了塔中Ⅰ号断裂带和塔中45井三维模拟区O〓灰岩的构造应力场和应变场,结果表明:研究区主应力方向为北东~南西向,第二期的构造扭动使其由北向东发生了一定的偏转,但总的方位变化不大;O〓~S~D时期,塔中地区构造运动较强,研究区大部分处于高应力状态,岩石破裂程度较高,而岩芯观察结果也证实了这一结果,即O〓灰岩地层中早期形成的构造结构面比较发育,单个结构面的规模也较大;C~P时期,岩石的破坏程度较早期有所提高,主要表现在两个方面,一是各局部区岩石的破坏程度普遍有所提高;二是各个级别破裂区的分布范围相应地扩大了;研究区应力分布表现出明显的不均匀性,特别是剪应力,无论是O〓~S~D时期,还是C~P时期,都有很大的差异性,特别是在小断层的端部,剪应力比较集中,而且在断层的两盘,剪应力方向和大小都变化极快。

In contrast, many geological, petrological and geochemical problems of H9 formation remain unsolved.

文中详细论述了这些火山岩石的结构构造、矿物成分和岩石化学成分,以及微量元素。

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