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构造层位     
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  tectonic layers
     Starting from the model the extraction of the relevant contour maps or cross section, as further utilization of reservoir model analysis, is a tool to predict the spatial relationships between faults and tectonic layers.
     从地质模型出发,提取相应层位的等值线图或横切剖面显示,是进一步利用储层模型分析来检测断层与构造层位之间空间关系的一种手段。
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  structural beds
     joint constraints by labeling of AVA synthetic records,evaluation of AVA inversion wavelet and logging and structural beds information can effectively reduce the issue of multiple solutions of inversion.
     通过 AVA合成记录标定、AVA反演子波估算以及测井、构造层位信息的共同约束 ,有效地降低了反演的多解性问题。
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  “构造层位”译为未确定词的双语例句
     Most moderate and strong earthquakes occurred in the gradient belt between different velocity blocks around middle crust,with strong inhomogeneity.
     大部分中强地震都发生在地壳中部附近不同速度体之间的梯度带附近,那里是深部介质分布最不均匀的构造层位
短句来源
     There exist different conditions of surface water and groundwater in different landform parts and tectonic locations where there are different karstification intensities and types at surface and in the depth.
     不同的地貌位置和构造层位具有不同的地表水和地下水状态,从而产生不同强度和不同形式的地表和地下岩溶。
短句来源
     Partial stack data retain original rich information. Restrained by logging and structural interperation results, initial model may be the most close to the actual underground conditions.
     部分叠加资料保留了原有的大量信息,在测井及构造层位的约束下,建立最符合地下实际情况的初始模型。
短句来源
  相似匹配句对
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
短句来源
     The X.
     在构造 X.
短句来源
     Gold mineralization is evidently controlled by stratigraphic horizon,structures and alteration.
     金矿化受层位构造、蚀变控制明显。
短句来源
     Its mineralization was mainly comtrolled by the intrusives,Stratigraphic beds and structures.
     其成矿主要受侵入体、地层层位构造控制。
短句来源
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It is thought to be the case that the migration, accumulation of natural gas must be closely related to the development of fracture in the compact sand-mudstone formation of some depression in Sichuan basin. In local structure, there always tends to be a transversal and longitudinal variations between reservoir beds and enriched gas-bearing zones. For the sole purpose of increasing the probability of hitting in drilling, research of seismic stratigraphy is conducted. The facies zone and tectonic level of interest...

It is thought to be the case that the migration, accumulation of natural gas must be closely related to the development of fracture in the compact sand-mudstone formation of some depression in Sichuan basin. In local structure, there always tends to be a transversal and longitudinal variations between reservoir beds and enriched gas-bearing zones. For the sole purpose of increasing the probability of hitting in drilling, research of seismic stratigraphy is conducted. The facies zone and tectonic level of interest are marked off. The channel for hydrocarbon migrating upward and potential well-developed fractured zone are delineated using the characteristics of seismic wave so that it may help exploit the oil/gas reservoir.

四川盆地的致密砂泥岩地层中,天然气的运移、储集与裂隙的发育程度密切相关。在局部构造上,储集层和含气的富集程度往往在横、纵向上会有变化。为了提高钻井的成功率,我们开展了地震地层学研究工作,划出了有利的相带和构造层位;并利用地震波的特征圈出油、气向上运移的通道及可能的裂隙发育带,以利于次生气藏的开发。 本文以地震资料的速度参数为基础,尽量利用其它可用的参数和波的特征,分析了凹陷东坡的一个局部构造。根据构造上第一口深钻井的气显示和地震资料的综合分析,进行了构造含气远景、特征及层位的宏观预测。应当指出,这种预测是建立在中间成果资料不断补充的动态过程之中,在推论中存在不够完善和不够严格的地方。本文的主要目的是强调普查勘探过程中,把地震成果和油、气直接挂钩,及时反馈信息,以便抓住战机,这应是当前地震勘探工作提倡和努力的方向。

Basic and uitrabasic rocks in the Dabie Group are exposed in the north of Dabie Mountain old fault-block uplift, Anhui Province. Lots of evidence show these basic and uitrabasic bodies were ophiolites, the relict fragments of oceanic crust. They evolved with the Dabie Group through one and the same orogenic movement.Because the ophiolitic bodies in this area had undergone intense structural deformation and metamorphism and later, extensive regipnal migmatization and lost their original features,it is very difficult...

Basic and uitrabasic rocks in the Dabie Group are exposed in the north of Dabie Mountain old fault-block uplift, Anhui Province. Lots of evidence show these basic and uitrabasic bodies were ophiolites, the relict fragments of oceanic crust. They evolved with the Dabie Group through one and the same orogenic movement.Because the ophiolitic bodies in this area had undergone intense structural deformation and metamorphism and later, extensive regipnal migmatization and lost their original features,it is very difficult to recove their original sequence. According to the present knowledge, the ophiolites can be clearly divided into the basal ultramafic complex and the mafic and ultramafic cumulates. The ophiolitic bodies are small, however, their numbers are great. They occur in the form of lens and are "the dismembered oghiolites".The ophiolitic zone is situated on the southern side of the Mozitan-Tongchen Deep-Seated Fracture deviding the Jinzhai-Huoshan Fault-Depression from the old fault-block uplift of the Dabie Mountain and extends nearly northwest-southeast in accordance with the regional tectonic lineament(schistosity) .The petrological and petrochemical features as well as the textural and structural characteristics of the ophiolitic bodies indicate that they are quite alike to the Alpine or the YaluZangbu ophiolites.Owing to the northward quick subduction of the oceanic lithosphere across the deep trench situated on: the southern margin of the North China Fault Block, the ophiolites were intensely compressed, crumbled aad emplaced onto different positions of the Dabie Group by the end of Middle Proterozoic.

在安徽境内大别群中出露一系列镁铁质和超镁铁质岩体,属于“肢解的蛇绿岩”。与大别群建造应属同一造山期产物。它们可能在中元古代末期,因洋壳海域的岩石圈断块沿华北断块南部的大陆边缘的深海沟向北快速俯冲消减,遭到强烈挤压破碎而侵位到大别群不同构造层位中。

The distribution of China's Sb-deposits is mainly controlled by tectonic structure.Some of themare also under the control of the lithological character and a certain stratum.In addition,a few ofthem are spacialy related to igneous rocks.In general,four Sb ore belts may be distinguished.It is:believed that most of the Sb-deposits were formed in the Yenshanian epoch,and a few of them in theIndo China and HimaIayan epoches.Based upon the structual,stratigraphic and litholgical characteri-stics mentioned in this...

The distribution of China's Sb-deposits is mainly controlled by tectonic structure.Some of themare also under the control of the lithological character and a certain stratum.In addition,a few ofthem are spacialy related to igneous rocks.In general,four Sb ore belts may be distinguished.It is:believed that most of the Sb-deposits were formed in the Yenshanian epoch,and a few of them in theIndo China and HimaIayan epoches.Based upon the structual,stratigraphic and litholgical characteri-stics mentioned in this paper,some suggestions on searching for large-scale and high-grade Sb-oredeposits in Chin are put forward.

中国锑矿床分布受大地构造控制总体可分为4个带,且与世界4个锑矿带相连。锑矿还受一定层位和岩性控制,少数在空间上还与火成岩有关。认为大多数锑矿形成于燕山期,次为印支期和喜山期。指出了根据构造、层位及岩性等方面如何在我国寻找大而富的锑矿床。

 
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