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Determining breakdown pressure in an anisotropic formation is important in oil and gas exploration and production.

准确计算各向异性地层中岩石破裂压力在石油勘探开发中有着十分重要的作用。

The structure of rock is extremely complicated discontinuous and heterogeneous body, its mechanics property has non-linear, anisotropism and rheology characteristic, which changed over time.

岩石的结构是极其复杂的非连续和非均质体,其力学属性具有非线性、各向异性及随时间变化的流变特性。

The anisotropy of rock is closely related to the migration and accumulation of oil and gas .

岩石的各向异性与油气的运移和储集有着密切关系。

Research and practice prove that there is obvious anisotropy in rock permeability.

研究与实践表明,由于受地质因素的控制,岩石渗透率的大小往往表现出明显的各向异性。

The key of studying this kind of complex system, is adopting the theory and methodology of complex system, combining the basic law of rock mechanics, found the scientific model and system info of complex system. To nonlinear, anomalistic geometry et.

对于这样的复杂性系统研究的关键,是采用复杂性系统的理论方法,并结合岩石力学的本质规律,采用适当的研究方法,建立复杂性系统的科学模型和理论体系。

A mass of pyrolite xenolith (such as peridotite andpyroxenide) and high-pressure mineral megacrysts (such as anorthoclase, augite and kaersutite)are found in cone sheets and BS volcanic rocks.

锥状岩席和BS火山岩包含有大量的上地幔岩石包体和高压矿物巨晶(歪长石、普通辉石和钛闪石)。

The anorthosite and similar rock types in the highlands and basalt lavas in the marea are the Moon's basic building blocks.

斜长岩和类似的岩石在高地典型,而玄武岩沉积在月球低地构成了月亮基本的建筑积木。

Composed mainly of anorthosite and plagiogranite, the leucocratic rocks show distinct Eu positive anomaly.

浅色岩类的岩石类型包括斜长岩和斜长花岗岩,它们均呈岩块状包裹于蛇纹岩中。

This conclusion, combined with the data obtained from the short-lived Hf-W and Sm-N d isotopic systematics, suggests that the Moon was initially accreted at 4.5 Ga, followed by development of the global lunar magma ocean. The primary lunar crust is composed by ferroan anorthosite which was produced by flotation of plagioclase during crystallization of the LMO. However, the mafic minerals, coevally crystallized with the plagioclase, sank to the base of the LMO due to their high density, and made up the main part of the lunar mantle, which served as the source during later mare basaltic magmatism.

根据这一年代资料,结合对月岩样品进行的短半衰期Hf-W与Sm-Nd同位素体系的研究结果,认为月球大致形成于45亿年,其后开始由岩浆海导致的内部核-幔-壳的分异,岩浆结晶的低密度斜长岩构成最初的月壳,而密度大的岩石构成月幔,而此月幔则成为后来月海玄武岩的主要岩浆源区。

The key factors to make the slide is controlled to make the model be similar in geometry, material and fabric with the antetype, then simulate the infection of river ,digging of road and so on, measure the data of the distortion of model, analyze the reason of the distortion and factors of the slide.

试验抓住造成滑坡的主要因素,根据所得的岩石力学参数及结构面参数,在几何条件、模型材料、结构面条件等方面都基本满足相似原理的情况下,对模型进行了河流下切、公路开挖等条件的模拟,测量观察边坡的卸荷回弹与层面的弯曲变形情况,利用所测数据分析论证滑坡的形成机制和影响因素。

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