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J31 Series Straight Side Presses Fixed is my company's traditional products, product stability and durability, with a loaded feature of moduli space, operation, maintenance is simple, suitable for punching, blanking, bending, stretching, correction, cold stamping and other techniques, both deep drawing, strong punching, extrusion and other functions.

J31系列闭式固定台压力机是我公司生产的传统型产品，产品稳定耐用，具有装模空间大特点，操作、维修简便，适用于冲裁、落料、弯曲、拉伸、校正、冷冲压等工艺，兼备深拉伸、强冲裁、挤压等功能。

The fold-and-thrust structure in the northwestern margin of the Junggar Basin is composed of the northern monocline belt,the middle syncline belt,the Ke-Wu faulted belt and the frontal slope belt,and is divided into the upper and lower structural layers in vertical.

准噶尔盆地西北缘冲断构造自西向东由北部单斜带、中部向斜带、克—乌断裂带和前缘斜坡带4个部分组成，在纵向又可划分为上、下两个构造层，上构造层的冲断序列要先于下构造层。

On the basis of plan form and crosscutting relationship of the faults, two kinds of tectonic systems were developed in Wu-Xia area, one was strike north-east, and another was strike east-west, the first was developed early and control the structural framework of Wu-Xia area, after that three times longitudinal compress action was happed. According to the intensity of tectonic deformation, The Wu-xia faulted zone from north to south can be divided into the thrust faulted belt, the fault fold belt and the monocline belt. from east to west have three regulatory faults, Wuerhe fault fold belt, Wuxia thrust faulted belt and Xiahong fault fold belt. Base on that 9 secondary structural unit can be divided.Structural accommodation zone and the distribution of reservoir strata have intimate business connection. Usually, Structural accommodation zone was the source zone of arenaceous sediment. The Wu-xia faulted zone have 3 kinds of structural accommodation, concordant approach, concordant overlap and concordant colinearity.

首先研究本区的构造特征，根据断裂的平面形态及相互切割关系，乌夏地区发育两种构造体系：北东向构造体系和近东西向构造体系，前者形成早，控制了该区的构造格局，晚期有3次近南北向挤压作用叠加；乌夏地区南北根据构造变形的强度不同分为冲断带、断褶带、单斜带，东西由于横向调节断层的存在分为乌尔禾断褶区、乌-夏冲断区和夏-红断褶区，进一步划分为九个次级单元；构造调节带与储集层的分布关系密切，通常是大量富砂质沉积的源区，乌夏地区发育三种类型的构造调节带：同向接近型、同向叠覆型和同向共线型。

Wuxia area was located on the eastern of northwest Junggar basin, it was a zone of bruchfalten affected by multiphase tectonic activity, have many faults and its fold morphology were very complicated, underwent three large structural activities, which happened in the late Hercynian movement, Indo-Chinese movement, and the Yanshan movement, by this,strata of Wuxia area can be divided into two primary tectonic sequences and seven secondary tectonic sequences, on plane, Wuxia area can be divided into three secondary structural units from north to south,they are foreland thrust belt, Wuxia fault fold belt and monocline belt, further, from west to east Wuxia fault fold belt can be divided into four fault fold belts.

乌夏断裂带位于准噶尔盆地西北缘冲断带东段，是一个受多期构造叠加影响的断褶带，断裂发育，褶皱形态复杂，自成盆期以来经历了海西、印支、燕山和喜马拉雅等多期构造运动，可划分为2个一级构造层序和7个亚构造层序，可划分出山前冲断带、乌夏断褶带、南部单斜带三个次级构造单元和四个更次一级的构造单元。

Hetian fault is the main fault which makes the nappe structure emplacement, and develops only in cover strata.

2和田断裂是中段和西段冲断带就位的主冲断裂，它仅发育于盖层中

Selibuya Fault has typical double structures and is composed of deep thrust fault and shallow and nappe thrust fault.

色力布亚断裂具有典型的双重结构，由深层逆冲断裂与浅层逆冲推覆断裂组成。

The structure in the east part was complex and violence and existed two separated nappe and thrust systems respectively formed in the north and south area.

逆冲推覆构造是西秦岭造山的主要构造形式，东部复杂，强烈，南北各有一个独立的逆冲推覆构造系统。

According to structural analysis and sediment comparison ,we judge the western of the basin is outside of west-edge thrust nappe belt .

盆地现今的西界为西缘逆冲推覆带所限，而西缘逆冲推覆带主要形成于晚侏罗世一白垩纪。

Behold the Chief who now commands Once more to serve his Country stands The rock on which the storm will beat The rock on which the storm will beat But arm'd in virtue firm and true His hopes are fixed on Heav'n and you-- When hope was sinking in dismay When glooms obscur'd Columbia's day His steady mind from changes free Resolv'd on Death or Liberty.

瞧，这是统帅我们的领袖，爲了国家他再次站了出来，坚强如风暴冲撃的盘石，坚强如风暴冲撃的盘石，但他以美德来武装，坚定而真诚，他寄希望于上帝和你们──当人们悲观失望的时候，当愁云笼罩着哥伦比亚，他意志坚定，毫不动摇，决心不获自由宁可死亡。

This method decomposes wave-front phase to a linear combination of orthonormal basis functions, According to the covariance of weight coefficient, a random wave-front phase is realized.

协方差冲激函数产生法对连续波前相位进行冲激函数正交分解，根据正交分解系数的协方差模拟平行光通过大气后的瞬时波前相位。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。