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geologic body造句

"geologic body"是什么意思  
造句与例句手机版
  • Three dimensional geologic body forward is a highlight of tem study
    三维地质体的正演是瞬变电磁法研究的一个热点。
  • Study on the theory of the software for visualization of the threedimensional geologic body
    三维地质体可视化软件理论探讨
  • 2d coupled hydro - mechanical elastoplastic finite element method for unsaturated geologic body and its application to analyzing bolting support
    应力耦合二维有限元方法及对锚杆支护的分析
  • Based on the nurbs technique and the theory of partition for geologic body , the 3 - d engineering geologic model for underground structures is established
    摘要工程区域地质条件是影响地下洞室群布置最主要的因素。
  • This paper puts forward the showing ways and the modeling algorithms for the familiar geologic bodies such as terrane , fold and faultage
    本文主要对常见的地质对象,如岩层面、褶曲、断层面等,提出了它们的表示方法和建立它们的三维模型的算法。
  • The place of the anomalous extremum of apparent resistivity curve is related to the position , thickness , resistivity and occurrence of geologic bodies ahead of the tunnel
    摘要在坑道电阻率超前探测工作中,视电阻率异常极值位置与异常体位置、厚度、电性以及产状相关。
  • Based on it the electromagnetic response under different depths of the 3 dimensional geologic body with different resistivities , magnetic conductivities and dielectric constants is simulated
    据此,可模拟计算任意具有不同电阻率、磁导率和介电常数的三维地质体在不同深度条件下的电磁响应。
  • By knowing the surface information of the geologic bodies , the planar section map and three - dimensional section map can be generated along arbitrary directions , which reflect the outer profile and inner structure of the geologic bodies
    提供了从任意方向对三维地质体剖切生成平面或立体剖面图的方法,使地质体的整体轮廓和内部结构得到直观的反映。
  • Using an olympic project as the paper analyzes various waveform features in the seismic imaging profiles , which are relevant to different backfills and geologic bodies in complex neritic backfilled areas , a prospecting example
    并通过奥运工程勘察实例详细分析了该方法在复杂的浅海人工回填区域中不同的填入物与地质体在时间剖面上所展现的各种不同波形特征。
  • Numerical simulation for 3 dimensional geologic bodies with different electric property parameters , which is conducted under the way of central loop tem , is the theoretical foundation for understanding its electromagnetic response characters and developing new interpreting methods
    摘要不同电性参数的三维地质体在中心回线瞬变电磁观测方式下的数值模拟是认识其电磁响应特征规律并进而开发新解释方法的理论基础。
  • It's difficult to see geologic body in a sentence. 用geologic body造句挺难的
  • 7 ) fractures belong to a complex geologic body with non - linear effect on reservoir ( s ) . well log parameters vs fractural development is also non - linear , hence , multi - parameter evaluation is adopted as necessary . the individual parameter evaluation is effectively employed for local part rather than for whole area
    裂缝是复杂地质体,对储层的影响是非线性的,测井参数和裂缝发育的关系也是非线性的,因此必须采取多参数联合评价的方法;单参数评价局部有效,应用于整体效果不佳。
  • And its spatial analytic functions such as overlay analysis and buffer analysis that can be used to extract multiple variables and information from geologic bodies organized in map layers in point , line or polygon shape are in favor of discovering ore - forming factors , summarizing regional metallogenic regularities and constructing geologic metallogenic models
    以矢量数据结构为主,实现了对点、线、面地质体的gis空间分析功能,以便对多元矢量数据信息进行叠加分析和相关分析,发现和归纳研究区域的成矿规律,建立成矿地质模型。
  • In the experiment , the hydrocarbons generated from pyrolysis are appropriately classified as drained and occluded hydrocarbons which correspond to the amount of hydrocarbons in geologic body entering reservoirs by primary migration and the amount occluded in parent rocks and evolving continuously together with parent rocks , respectively
    试验中把热解生成烃适当分成排出烃和滞留烃,分别对应于地质体中油气经初次运移进入储层的量和滞留于母岩并同母岩一同继续演化的量。
  • ( s ) weathering and unloading action which are the two main exogenous process is active in epigenetic - surface . so , although one is different with the other , they are associated with each other closely and are cntrolled by geostress and seepage fields . in fact , weak weathered zone corresponds to weak load - off one , strong weathered zone corresponds to strong load - off one in virtue of result of this dissertation . ( 6 ) rock mass is a geologic body which is composed of rock and structural plane . and under the condition of geostress . temperature and seepage fields , correspondingly . studying weathering should pay attation to the aspects of rock , structural plane and fields . according to this . the author subdivises rockmass weathering into rock weathering and structural weathering , ulteriorly , the dissertation studies rockmass weathering from three aspects as follows : ? ock weathering : aberrance degree of mineral and physical mechanical performance of weathered rock ; ? e have already knew that weathering action damage the integrity of rock mass , but few applies it to engineering practice . the dissertation is based on trend o
    本文研究结果为弱卸荷与弱风化大致对应、强卸荷与强风化大致对应; ( 6 )岩体是由组成它的岩石与缺陷赋存于一定环境场中的地质体,据此本文将岩体风化细划为岩石风化与结构面风化,并进而将表征岩体风化的指标相应地归结为三个方面来加以研究并应用于工程实践,这就是:对于岩石风化,主要为矿物的变异程度与风化岩石的物理力学性能研究:虽已认识到风化作用破坏了岩体完整性,但将该理论应用于岩体风化分带却不多见,本文即从浅表部位硬性结构面间距、条数、迹长、块度等随远离临空面的变化规律来研究岩体风化分带:不同风化、卸荷程度的岩体实际处于不同环境场中,弹性波速变化与特定环境场相对应,因而是反映岩体风化、卸荷的综合因素。
  • The generation of hydrocarbons can be divided into four stages with continuous evolution , from unmature to overmature stages , and the migration into three concentrated stages ; that is , the geological process of geologic body during which hydrocarbons generate and migrate simultaneously is simulated as multistage generation and concentrated migration , thus , the possible distribution of hydrocarbons in reservoirs in different evolutionary stages and under different migration efficiency can be obtained
    从未熟到过成熟阶段将油气的生成分成4个连续演化阶段,运移分成3个集中阶段,即用多阶段生成、集中运移模拟地质体中油气边生边运的地质过程,得到了不同演化阶段不同运移效率下储层中可能的油气分布。
  • Comparative studies of ree geochemical characteristics of various geologic bodies in the deposit indicate that the various ores and alkaline volcanic rocks contain abundant ree , specially lree the chondrite - normalized patterns of both ores and alkaline volcanic rocks show a strong lree enrichment and positive eu anomaly , in contrasting with the dolostones which show slight lree enrichment and moderately negative eu anomaly
    同期成矿流体从早期到晚期(块状矿石条带状矿石) ,轻重稀土分异变小,稀土总量增加,条带状矿石中稀土含量最高;矿石黄铜矿6345值变化在一0 . 3编到2 . 8 % 。范围,显示慢源硫特征;菱铁矿6 ’ 3c ( 8 % 。
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