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foliation相关的网络例句

查询词典 foliation

与 foliation 相关的网络例句 [注:此内容来源于网络,仅供参考]

Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of m in eral gra in s in the rock.

片理化断层岩石具有发育良好的面理构造,这些面理是岩石中矿物颗粒优选定向而造成的。

Foliation: It generally refers to any plane structure developed in a geological body, normally divided into two origins, primary and secondary.

面理:泛指地质体中发育的具有面状形体的面状构造。

The foliated rock belt is over one hundred meters in width and the intensity of foliation in the center is stronger than that in the margin.

这个片理化岩带有100多来宽,带中央岩石的片理化程度较之于带边缘岩石要强。

These rocks are lack of foliation and resulted from the brittle fragmentation of mineral grains with rotation of grain fragments accompanied by fractional grain boundary sliding and dilatancy.

这类岩石缺乏面理构造,是由于矿物颗粒的脆性碎裂,旋转以及颗粒边界的磨擦滑动和扩展而造成的。

These rocks are lack of foliation and resulted from the brittle fragment ation of mineral grains with rotation of grain fragment s accompanied by fractional grain boundary sliding and dilatancy.

这类岩石缺乏面理构造,是由于矿物颗粒的脆性碎裂,旋转以及颗粒边界的磨擦滑动和扩展而造成的。

Whereas foliation attitude of gneiss type exerts a relatively weak role in controlling attitude of miniature faults in gneiss type rocks.

而片麻岩类岩石叶理产状对发育于该类岩石内的微断层产状控制作用相对较弱。

It's considered that seismic velocity of metamorphic rock is related to metamorphic type and strength, density, lithology and geologic structure, at the same time, intense foliation structure and interlayer of rocks different in velocity make seismic velocity present obvious anisotropy and transverse imhomogeneity.

研究认为,变质岩的地震波速度与变质作用类型和强度、岩石密度、岩性及构造有关,同时由于该区超高压变质岩的面状构造发育,而且不同地震波速度的岩石在空间上表现出明显的迭置关系,因此地震波速度呈现出显著的各向异性和横向不均匀性。

A sheath fold looks like a scabbard or human's tongue. Its fold axial plane or flatten ed plane is parallel to the foliation and there is strong stretching lineation on the sheath fold.

鞘褶皱看起来像一把鞘或是像人的舌头,它的褶皱轴面或压扁面是平行岩石中的片理面的,鞘褶皱上有强烈的拉伸线理。

The major methodology is the structural analysis of crusted and lithosphere structures. The subject emphasize on the study of the basic characteristics, observation methods of small to middle scale structures. The course introduces the origin of fault, fold, joint, foliation and lineation, and the research method and thinking of modern structural geology.

构造地质学以构造分析作为研究地壳或岩石圈构造的方法论,主要研究中、小型尺度的基本构造特征、分类和观测方法,介绍断层、褶皱、节理、叶理和线理构造成因机制的基本理论及现代构造地质学的研究方法和思路。

While the nearly E-W-trending steeply dipping foliation belts and their corresponding structure of metamorphic strata are attributed to the second orogenic cycle.

而近东西向陡倾叶理带及相应的变质地层结构则属于后期造山旋回。

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