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   projection map 的翻译结果: 查询用时:0.197秒
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projection map
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  投影映射
     Under general feasible set,in consideration of the algorithms for nonsmooth equations and the properties of projection map,the algorithms using the normal equation to solve are discussed.
     在一般可行集下 ,结合非光滑方程组解法及投影映射的性质 ,讨论了法方程求解变分不等式问题的算法构成 .
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  “projection map”译为未确定词的双语例句
     Electron crystallographic analysis of MII crystal shows a lattice with parameters of a =20 6(±0 1) nm, b =16 1(±0 1) nm and γ = 90(±1)°, and the projection map with P2 symmetry is produced at the resolution of 2 06 nm.
     进一步的电子晶体学分析表明 ,MII晶体的晶格参数为 :a =2 0 6 (± 0 1 )nm、b =1 6 1(± 0 1 )nm和γ =90 (± 1 )°,其投影图的分辨率为 2 0 6nm ,并具有P2对称性。
短句来源
     A new pattern recognition method called the optimal map recognition(OMR)method has been proposed to select the optimal projection map among various pattern recognition maps.
     提出了一种新的模式识别方法———最佳投影识别法(optimal map recognition method) ,该方法可从已知模式识别投影图中筛选出最佳的一个.
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     The optimal projection map can be used for the computer aided molecular sieving of N (3 oxo 3,4 dihydro 2 H benzo[1,4]oxazine 6 carbonyl)guanidines. The designed samples with probably high Na/H exchange inhibitory activities were determined in such a way that their representing points should be in the optimal region formed by the OMR method.
     将该方法应用于N(3氧3 ,4二氢2 H苯并[1 ,4] 嚙嗪6羰基) 胍类化合物的Na/H 交换抑制活性的分子筛选,得到了建模所用的最佳模式识别投影图,在此基础上形成的判据可用以筛选得到具有较高Na/H 交换抑制活性的该类新化合物
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     . The projection map of the negatively stained two_dimensional crystal of LHC_Ⅱ complex shows that the crystal has p3 symmetry, lattice constant 15.4 nm×15.4 nm, which is different from the LHC_Ⅱ of spinach (Spinacia oleracea L.)
     负染样品的二维投影结果表明 ,该晶体为p3对称性 ,晶胞参数为 15 .4nm× 15 .4nm ,不同于以往报道的菠菜 (SpinaciaoleraceaL .)
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     It adopted 2-level projection maps which were Free Space Map and Detail Projection Map to locate 2D position of avatar during collision detection;
     二级平面投影图Free Space Map 和Detail ProjectionMap在不同阶段提供化身的空间信息;
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  相似匹配句对
     RESEARCH ON MAP PROJECTION COMPONENT
     地图投影组件化研究
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     Projection Transformation of Raster Map
     像素地图的投影变换
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     A and MAP.
     MAP.
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     INTERNET MAP
     网络地图
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     On Projection Teaching
     浅谈投影教学
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  projection map
If W is the Weyl group of G and e, f ∈ Λ with e ≤ f, we introduce a projection map from WeW to WfW.
      
The range projection map is, up to a Jordan homomorphism, the only natural map from the spectral lattice onto the projection lattice.
      
In operator algebra theory, a conditional expectation is usually assumed to be a projection map onto a sub-algebra.
      
The projection map seems to indicate an enzyme conformation somewhat similar to vanadate-induced crystals but different from lanthanide-induced crystals of Ca2*-ATPase.
      
Ca2+-ATPase molecules appear as quasi-triangular blobs in the projection map and seem to form dimers.
      
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This paper introduces three Kinds of methods to arrange drill holes on the pitching orebody.1).Projection method of plunge-line.According to orebody surficial attitude,we can obtained the projection range of deep-seated orebody by stereog-raphic projection, and then arrange drill holes.2).Axial-line method of orebody:At first work out the patterns of every level horizontal projection of orebody to find its axial-line,then arrange drill holes based on the downward- extending orientation of this line.3)Longitudinal...

This paper introduces three Kinds of methods to arrange drill holes on the pitching orebody.1).Projection method of plunge-line.According to orebody surficial attitude,we can obtained the projection range of deep-seated orebody by stereog-raphic projection, and then arrange drill holes.2).Axial-line method of orebody:At first work out the patterns of every level horizontal projection of orebody to find its axial-line,then arrange drill holes based on the downward- extending orientation of this line.3)Longitudinal projection method: According to orebodies in control drill holes,orebody boundaries will be delineated on longitudinal projection map and drill holes can be arranged by this map combined with exploratory profiles.

本文介绍侧伏矿体的三种布孔方法,1)倾伏线投影法:根据矿体地表产状用赤平投影等方法求出矿体延深的投影范围,然后布孔.2)矿体轴线法:先编制矿体各中段水平投影图,求出矿体轴线,然后根据该轴线下廷方向布置占孔.3)纵投影法:根掘控制孔见矿情况,在纵投影图上圈定矿体边界,用此图结合剖面图布置占孔.

The fault effect produced by moving ore bodies by fault results in "overlapping" or "opening" of the ore bodies on the horizontal projection map. The accuracy of the reserve calculation should be affected without consideration to the effect.Therefore,the horizontal projection location of the crossline between ore body and fault, that is the area of "overlapping" or "opening" must be decided.The cross form between ore body and fault is changable, but the real relation forms are just two types, those...

The fault effect produced by moving ore bodies by fault results in "overlapping" or "opening" of the ore bodies on the horizontal projection map. The accuracy of the reserve calculation should be affected without consideration to the effect.Therefore,the horizontal projection location of the crossline between ore body and fault, that is the area of "overlapping" or "opening" must be decided.The cross form between ore body and fault is changable, but the real relation forms are just two types, those are same direction cross form with acute angle and same direction cross form with obtuse angle. Two formulas have been obtained by deducing the geometric figures and numbers, which can be used to calculate the horizontal projection location of the crossline between ore body and fault. It is helpful for the reserve calculation.

断层错动矿体产生的断层效应导致水平投影图上的矿体“重叠”或“拉开”,如不考虑此效应,进而影响储量计算的准确性。所以必须确定矿体与断层交线的水平投影位置,即“重叠”或“拉开” 的区域。矿体与断层相交的形式多样,但真正的关系类型只有两种,即相向锐角相交式和相向钝角相交式。对它们进行几何图解和数字推导得出的两个公式,可以用来计算矿体与断层交线的水平投影位置,对储量计算起帮助作用。

The fractured gas reservoirs in east Sichuan,no matter they are anticline traped ones or structuralfracture pinch traped ones,are all controlled by tectonic deformation.The hydrocarbon enrichment isclosely ralated to Himalayan tectonic evolution.The tectonic evolution of the present region inHimalayan orogen has always been disputed,and the division of formation stages differs from eachother.Therefore,the evolution in hydrocarbon-bearing structurs may also be different.In application of structural geometric...

The fractured gas reservoirs in east Sichuan,no matter they are anticline traped ones or structuralfracture pinch traped ones,are all controlled by tectonic deformation.The hydrocarbon enrichment isclosely ralated to Himalayan tectonic evolution.The tectonic evolution of the present region inHimalayan orogen has always been disputed,and the division of formation stages differs from eachother.Therefore,the evolution in hydrocarbon-bearing structurs may also be different.In application of structural geometric and directional filter analysis,the structures can be divided into four fold sys-tems in this paper according to the folds strikes,the dipping direction of pivots,the closure,cross-sectionpattern,amplitude and depth of folds as well as the configuration on sterographic projection map.Thenthe evolution of these folds is divided into four generation based on the alternative relationship of bigand medium sized folds and the displaced fabric type of the pivots of small sized folds.The distributionand superimposition of the fold systems in south,north and central blocks differ greatly from eachother due to the control of two northwest strike basement rifts.Through rebuilding tectonic evolution history,the authors consider that,traps formed earlier havethe priority to trap oil and higher enrichment,conversely,the enrichment may low;synclines that up-lifted higher in amplitude and emerged older in strata may have poor preservation condition,otherwise,the condition may good.Exploration in this area has proved that the ratio of success can reach 75%for the wells located according to the above mentioned.

川东地区的裂缝性气藏,均受构造变形特征所制约。作者应用构造几何分析与定向滤波分析相结合的方法,将本区构造划分为四个褶皱系和四个世代,均属喜山期形成。并认为:形成早的构造(圈闭)气藏富集程度高,反之则低;隆起幅度高、出露地层老的背斜气藏的保存条件差,反之则好。按此法部署探井的构造,钻探成功率达75%。

 
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