Character appearance of fault structure in seismic wave CT inversion for mine work faces detecting;
断层构造在矿井工作面震波CT反演中的特征显现
The technique of "balance section" is a combination of geological thought and computer technique, which improves the research for fault structure up to quantitative stage.
平衡剖面技术是地质思维和计算机技术的结晶,使对断层构造的研究提高到定量阶段,其依据是在垂直构造走向的剖面上,地层长度和面积(2D)或体积(3D)是均衡的。
To show stratum-structure in basin,a new kind of method is presented and an algorithm is provided to realize the method,which is based on some recent advancement in theory research.
针对地质体建模中的地层-构造恢复与数据更新问题,提出了一种适合重现地下地层-构造格架的方法,并给出了相应的实现算法。
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
研究结果表明,前陆盆地内发育有两种层序模式,即构造层序和气候层序。
The structural sequences of stretch rift basin is usually composed of coarse grain sequence in the bottom,volcanic rock bearing sequence in the lower part,deep water sequence in the mid part and filling sequence in the upper part.
伸展裂谷型盆地的构造层序由下而上一般由底部粗粒层序组、下部含火山岩层序组、中部深水层序组和上部充填层序组组成 ,南堡凹陷据此可划分出 6个构造层序 ,其中第三、四构造层序控制了南堡凹陷两期主要的含油气系统分布。
Integrated information about geology, geophysical and assaying, study structural sequence and sedimentary system of transition period of fault sag in Jiyang depression.
运用地质、地球物理和分析化验等综合资料,对济阳坳陷的断-拗转型阶段的构造层序及沉积体系作了系统的研究。
Renewing knowledge of deep structures of Dongying depression.;
重新认识东营凹陷的深层构造
The orientation and amplitude of thinning and thickening zones of main mining coal seams in some mining areas of Qianling coal mine are studied,through observation and research on the features and distribution regularities of slip sheet structures.
通过对前岭煤矿部分采区层滑构造形态特征及展布规律的观测和研究 ,分析了该地段主采煤层薄化带及增厚带的展布方向和幅度 ,揭示了 31～ 5煤层组中 ,软弱夹层及滑动构造发育情况 ,指出 4煤层变薄及增厚的规律性 ,为矿井安全提供了超前地质信
By relating the maximum reflectivity (R°max%) of the vitrinite to the coal seam stru-ture breakage in Sudong Coal Mine Area, the authors draw the conclusion that the increase of the maximum reflectivity of the vitrinite can be attributed to the structure breakage cuased by the slip sheet structure and the large quantity of heat resulting from it.
本文在分析宿东矿区煤的镜质组最大反射率(R°_(max%)值与煤的构造破坏关系的基础上,指出层滑构造使得煤层发生破碎,并产生大量的热量,是引起本矿区镜质组反射率值增加的重要原因。
ANALYSIS ON THE INFLUENCE OF FAULT STRUCTURE TO WATER-INRUSH FROM COAL FLOOR
断层构造对煤层底板突水的影响分析
Research of Isoline Drawing with Faults Algorithm Based on Geoview System;
基于GeoView系统带断层构造等高线图绘制算法研究
Structural evolution of Shigang Fault and features of hydrocarbon accumulation in Jinhu Sag
金湖凹陷石港断层构造演化及油气聚集特征
From Fold to Fault-the Concept Change on Structural Forms
从褶曲到断层——构造形态认识的转变
Application of the Fault State Equation in Mine Structure Analysis
断层型态方程及在构造分析中的应用
Classification of Faults in the Zhongwei Fault Zone and Its Tectonic Implication
中卫断裂带断层类型划分及其构造意义
If the strike of a fault is parallel to the general trend of regional structures, it is called longitudinal fault
如果断层走向与区域构造的总体走向相平行，就称之为纵向断层;
If the strike of a fault is perpendicular or diagonal to the trend of regional structures, it is refer to transverse fault.
如果断层走向与区域构造线走向相垂直或斜交，则称之为横向断层。
And the places where these plates come up against one another are called faults in the earth's crust.
构造板块挤在一起的地方，就叫做地壳的断层。
Because the faults are colossal and very directive, the horst structure is developed.
由于断层规模大，方向性强，致使地堑构造发育。
Through long terms of tectonic evolutions, it changed into a transform fault in the Cenozoic Era.
经长期构造演化于新生代转变为转换断层。
The Study of Mineralization by Relay Structure of Normal Fault on Typical Metal Ore Deposit;
典型金属矿床正断层中继构造控矿作用研究
The Research of Medical CT Image s 3D Reconstruction and RP Manufacture;
医学断层影像三维重构与快速成型制造的研究
Evaluation and Analysis of Active Faults and Regional Tectonic Stress Field of Hebei Plain;
河北平原活断层评价及区域构造应力场分析
Structural Style and Thrust Breakthrough Model of Fold in Southeast Guizhou
黔东南地区褶皱构造样式及其断层突破模式
Mechanics Analysis of Normal Fault Formation and Control of Structure Coal
正断层形成的力学分析及其对构造煤的控制
Constraints of Paleozoic Normal Faults on Structural Characteristics in South Guizhou
黔南地区古生代正断层对构造特征的制约
QUATERNARY FAULTS AND NEOTECTONIC MOVEMENT IN THE YANGTZE RIVER ESTUARY
长江口海域的第四纪断层与新构造活动