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1)  Shanshen structure
鄯深构造
1.
According to the post_drilling evaluation in Shanke?1, Triassic oil_accumulation conditions for Shanshen structure are analyzed from several aspects, such as oil_source correlation, source maturation correlation, reservoir development, secondary porosity, seal characteristics, trap evolution history, and hydrocarbon migration direction and pat.
依据鄯科 1井的钻后评价成果 ,从油源对比与烃源岩演化、储层发育特征与次生孔隙形成机理、盖层特征、圈闭演化历史、油气运移方向及通道等多方面分析了鄯深构造三叠系油藏的成藏条件 ,并指出鄯善弧形带和葡北构造带是台北凹陷深层下一步油气勘探的较有利的区
2)  deep structure
深部构造
1.
The special bouguer gravity fields and the deep structure in yinshan-daqingshan mountains;
阴山大青山山系特异重力场与深部构造
2.
The feature of deep structure in the area is revealed, and the deep metallogenesis is discused.
本文中利用重力、航磁和深部地球物理剖面资料,解析研究区三维岩石圈结构,揭示深部构造特征,进而探讨深部成矿作用。
3.
By analysing and studying aeromagnetic and gravity anomalies and theirtransformed results,this paper explains the distributing characteristics of deep structures,such as folds and fauIts,granite bodies,the Archean coplex in Qingyuan area and therelations between these deep structures and gold deposits.
通过航磁、重力异常及数据处理成果的分析和研究,阐述了清原地区深部构造、区域构造、花岗岩体及太古宙变质杂岩的展布特征与金矿成矿之间的关系,指出了该区金矿成矿的远景地段。
3)  deep structure
深层构造
1.
Renewing knowledge of deep structures of Dongying depression.;
重新认识东营凹陷的深层构造
4)  Deep-seated structure
深部构造
1.
A preliminary interpretation on the deep-seated structure of the Longgang compound landmass;
龙岗复合陆块深部构造浅析
2.
On this basis, the authors focused on the upper mantle lithosphere-asthenosphere structure of eastern China, and concluded the following: (1)seismic tomography images can diotinguish between Mesozoic and Cenozoic deep-seated structures,using di.
文中以地震层析原始数据为基础,结合大地电磁测深和热流值数据,对老资料重新开发,编制了中国东部岩石圈厚度图、大地热流值图、岩石圈构造与矿集区关系图等,在此基础上对中国东部上地幔岩石圈-软流圈构造及其变异进行了初步研究,认为:(1)中生代燕山期较大型深部构造(如软流圈上涌体)的地震层析影象可存留至今,运用大地热流值及其相应浅表岩浆岩、矿集区等特征差异可以将中、新生代深部构造加以区分;(2)中国东部深部构造总特征:上地幔岩石圈-软流圈构造起伏变化,岩石圈西厚东薄,软流圈上涌发育且形式各异。
3.
Based on the great change of the lithosphere thickness,the geothermal flow and Moho surface,and epigenetic magma structure activities,the sketch map of deep-seated structure of North China is constituted,and the relationship model of Yanshanian upwelling of asthenosphere and lithosphere structural activity is built.
通过岩石圈厚度变化、大地热流值和莫霍面起伏,结合浅表岩浆构造活动,编制了华北地区深部构造略图,建立了燕山期软流圈上涌与岩浆构造活动的关系模式,总结了该区的深部构造特征:岩石圈厚区与软流圈上涌区共存。
5)  texture depth
构造深度
1.
so it s completely viable that the method of laser cross section instrument replaces the method of handmade spreading the sand on the examination of texture depth.
通过300多公里的路面抗滑性能比对检测,发现激光断面仪法与手工铺砂法具有良好的相关性,因此,用激光断面仪法代替手工铺砂法进行构造深度检测是完全可行的。
2.
25% and the texture depth being more than 1.
25%,构造深度在1。
3.
The non-segregated area texture depth can be predicted using various properties of the original job-mix formula.
通过现场和室内试验检验国外2个沥青路面均匀区域构造深度预估模型的适用性,结果表明这2个模型都存在一定的缺陷。
6)  structure depth
构造深度
1.
Through lots of experiments for the factors that gravel grading and asphalt amount in asphalt concrete influences their porosity and structure depth.
通过大量室内试验研究了沥青混凝土矿料级配、沥青用量等因素对其体积性能(空隙率)和表面特性(构造深度)的影响。
2.
Based on the analysis and description of vertically-l ayered property of the fault,the conception of"structure depth" has been propo sed for the first time,which may be used to describe the position in vertically -layered section for certain place of the fault.
在分析和论述断层垂直分带性的基础上 ,首次提出了“构造深度”这一概念 ,用以描述断层某处在垂直分带中的位置 ,指出与断层的性质、时代、岩性、规模一样 ,构造深度也是决定断带特征及其水文地质条件的主要因素之一。
补充资料:热深厥深
热深厥深 热深厥深   病证名。指热厥证的征象。指邪热越深入,四肢厥冷的症状越严重,皆因阳气被遏,邪气内闭所致。属真热假寒证。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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