地质构造运动

地应力场与地质构造运动关系研究

Study on the relationship between in - situ stress field and tectonization

为进一步研究本地区地质构造运动的演化规律提供了依据。

The results also contribute to researching into the evolutional regularity of the tectonic movement .

深反射地震剖面的解释要着眼于大的地质构造运动和成因，运用地质规律进行综合地质解释。

The interpretation of the deep reflection seismic profile should be focused on the large geological tectonism and its genesis ;

裂缝的形成与构造运动有关，并可以提高岩石的渗透率。地应力场与地质构造运动关系研究

Fracture is mainly formed with tectonization and increases permeability . STUDY ON THE RELATIONSHIP BETWEEN IN - SITU STRESS FIELD AND TECTONIZATION

自然干扰因子包括地质构造运动、气候及水文改变等，人为干扰因子主要是指农业政策、人口压力、水利工程及环境污染等。

Natural disturbance factors included tectonization , climate , hydrological change and so forth . Human-caused disturbance factors included agricultural policies , population pressure , water conservancy , environmental pollution and so on .

本文根据地质构造运动是产生构造应力的主要原因，提出采用模拟构造运动的位移边界条件方法拟合初始地应力场，给出了一种用位移边界条件拟合初始地应力场的方法。

A new practical analytical method is presented to simulate the initial geostress which uses the displacement as boundary condition in FEM , based on the fact that tectonic stress is produced by tectonic movement .

地壳形变是研究构造运动的一种有效手段，它是地质构造运动的直接结果和外部表象，明显地受到浅部构造的控制。

Crustal deformation is a valid method that studies geologic tectonic movement , it 's a kind of direct result and exterior idea of geologic tectonic movement , obviously subjects to the influence of shallow tectonic .

历史时期内，黄河下游河道多次迁徙，河道的走向与新的地质构造运动有关，多沿新构造运动所形成的活动断裂线分布，呈西南东北、东西或西北东南向。

The course of the lower Huanghe River changed many times in history . The strike of the course is related to the new tectonic movement , that is distributed along the active fracture line formed by new tectonic movement in the direction of southwest-northeast , east-west or northwest-southeast .

珠江三角洲地区的基岩地质、新构造运动、航磁和重力资料都反映NEE向是最主要的构造方向，NEE向的恩平－海丰一线把研究区分成南北两区。

The NEE striking faults are the main active fults in the Pearl River Delta area . The study region may be divided into the south part and north part with a Haifeng-Enping line in the direction of NEE .

台湾海峡地震与地质构造、地壳运动的关系

Earthquakes in Taiwan Strait and its relationship to geological structure and crustal movement

长江中游自然环境的对称性是由区域地质构造和构造运动控制的。

In addition , areal geology structure and tectonic movement control the symmetry of natural environment .

地质流体与构造运动

Geology fluids and structure movement

永春地热田热资源赋存规律是其特殊地质构造制约地下水运动的结果。

Preservative law of geothermal resources of Yongchun is result of ground water movement under controlled by special geological structure .

由于地质构造、地质运动及所受各种采矿活动扰动的复杂性，使得冲击地压的定量预测成为一个比较困难的问题。

Because geological structure , geology movement and complexity of various kinds of mining activity perturbations , it 's more difficult problem to quantitative predicted on rockburst .

通过对龙门地热田地质构造、地下水运动特点及规律的研究，提出了在地热田内寻找地下热水的富水靶区，并推算了其范围。

Through a study on geological structure , ground water movement features and patterns in Longmen geothermal field , the paper set forward a geothermal water productive target area , and predicts its extension as well .

本文对晚新生代贵州喀斯特地貌演进的三大控制因素，即地质基础、新构造运动及挽近气候波动进行了分析论证。

In this paper , three determined factors influencing on the evolution of karst geomorphology of upper Cenozoic in Guizhou , e.g. geological basis , neotectonic movement and neoid climate fluctuation are discussed .