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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。

The study of glacial structure will extend the topics of glaciology, and make a contribution to construct the physical and mathemtical models of deformation of rocks.

冰川是地壳上重要的地质体之一,开展冰川构造的研究不仅丰富了冰川学的研究内容,而且也开拓了构造地质学的研究领域。

The study level of tectonic environment is not high for the phase of Neoproterozoic to early Cambrian in the study area, lacking combined foundation of sedimentation, stratigraphy, petrology and geotectonics.

研究区新元古代-寒武纪早期构造环境的研究程度较低,缺少沉积学、地层学、岩石学和构造地质学的综合研究基础。

The sealing degree was firstly evaluated based on the sealing characteristics of the faults transversally and longitudinally, by means of comprehensive assessment of fuzzy mathematics.

本文以胜坨油田坨30断块沙二段油藏为例,运用现代地层学、沉积学、构造地质学、储层地质学及油藏工程学等多学科的理论和方法技术,针对胜坨油田坨。。。

The high-grade metamorphic terrain of Hengshan located at the hinderland of North China Carton in northern part of Shanxi province, China, is a middle-lower crustal transition area of the typical continental crustal profiles of the Wutaishan—Hengshan—Datong—Jining of the early Precambrian etamorphic terrain in China.The Hengshan gneisses of the amphibolite—granulite facieses metamorphic terrain consist of the TTG gneisses and the horizontal adding mantle materials. The Supracrustal rocks in this area are composed of the mafic volcanic rocks and sedimentary rocks. The plenty of granitoid magma activities are the result of anatexes.

中文题名恒山中深变质岩区构造样式副题名外文题名 Tectonic styles of the high-grade metamorphic terrain of Hengshan 论文作者苗培森导师宋鸿林教授学科专业构造地质学研究领域\研究方向学位级别博士学位授予单位中国地质大学学位授予日期2001 论文页码总数88页关键词中深变质岩区构造地质恒山区域构造地质馆藏号BSLW /2003 /P548 /4 位于华北克拉通近中部的恒山中深变质岩区,亦即恒山高级变质岩区,是从五台山—恒山—大同—内蒙集宁这一浅变质岩区至中深变质岩区的我国早前寒武纪典型大陆地壳剖面代表中下地壳过渡带的地区。

In this dissertation, sedimentology, historical geology, structural geology, geophysics, structural dynamics/geometric, plate structure etc were combined properly. Taking Jiyang depression as studying object, fault distribution of different periods was analyzed, and thus discussing their structural dynamics. Using tectonic subsidence history modeling and denudating relationship between hanging wall and foot wall in Mesozoic faults, fault activity characteristics were discussed.

本论文将沉积学、地史学、构造地质学、地球物理、构造几何学和运动学、板块构造等多学科有机的结合,以济阳坳陷为研究对象,采用各时期断裂分期配套,分析了不同构造运动时期济阳坳陷断层展布,进行构造运动学讨论;利用构造沉降史模拟与中生代断层上下盘剥蚀关系的恢复,探讨了中生代断裂活动的特征。

Determination of depth of granitic plutons was helpful for understanding of uplift of terranes and deep tectonism.

同时,构造地质学和大地构造学自身的研究也将不断拓宽研究领域①,如:1不断拓宽研究的时空尺度,深入了解地球早期构造作用和大陆地壳深部构造作用;2精确确定变形特征,特别是流变学特征,估算应变强度和流变学参数;3精细测定变形的时代,特别是早期变形的时间;4深入分析构造发生的动力源问题。

Structural geology seeks to approach its subject of study in a quantitative way.

构造地质学与其他科学一样以定量化作为其目标之一,构造的应力分析和应变分析是构造地质学定量化发展的手段。

This view has practical guidance significance for the petroleum,engineering and mineral prospecting sectors and also deepens the understanding in the theoretical study of structural geology.

该认识对石油、工程和找矿部门具有实际指导作用,对构造地质学的理论研究具有深化认识的意义。

Application of structural geology and rock mechanics, all kinds of geology nature of rock mass which are controlled by joint were discussed, at the same time, the paper analyzed structural trace and its geology influence factors.

运用构造地质学的原理和方法并结合岩体力学理论,描述了研究区受结构面控制的岩体的各种地质属性及其构造环境,本文中构造环境着重于岩体结构面的分析及地应力研究。

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