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砂带

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After five years of development,plastic products factory has become the industry's first "one-stop" supplier of underwear accessories, products covered by transparent straps, strapless matte, diamond straps, printing aiguillette, silicon plastic straps, bra oil bag, elastic band, bust back clasp, buckle plastic package, breasted, and many other varieties.

经过五年的发展,振泰塑胶制品厂已成为同行业中首家"一站式"内衣辅料供应商,产品涵盖透明肩带,磨砂肩带,钻石肩带,印花肩带,硅胶肩带,文胸油袋,松紧带,胸围背扣,包胶扣,排扣,等多个品种。

I used the band saw to cut them out, and a band sander to contour the edges.

我用带锯削减出来,并带砂光机,以轮廓边缘。

The mechanical cleaning can be done by using a shaving device, a sanding machine or a belt sander.

机械清洗可以使用打磨设备、喷砂机或者带式砂磨机。

Generally, the sedimentary microfacies that have fine grains, such as bank and crevasse splay, have much more clay minerals than the sedimenta ry microfacies that have coarse grains, such as under-water branched channel an d debauch bar.

与粗粒组分微相带(如水下分支河道、河口砂坝等)相比,细粒组分微相带含有较多的黏土矿物,从而具有较强的水敏、速敏及酸敏性。

Methods The implants were divided into sandblasted and dual acid- etched treatment Group and sandblasted, dual acid- etched, H2 O2 and heat treatment Group, and randomly implanted into distal - cordis end of each femur of the rabbits.

方法种植体分为喷砂、双重酸处理组和喷砂、双重酸、双氧水、热处理组,然后随机植入兔子股骨远心末端,2、4、8周后制作带种植体的骨组织样品。

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。

The absorption spectrum center wavelength of dolomite is near 232 μm is shorter than 235 μm of limestone,and thus RBD7 and RBD8 can be employed effectively to identify dolomite and limestone,respectively. Felsic rocks show AlOH and Fe3+ absorption characteristics in the VNIRSWIR region,while the maficultramafic rocks show Fe2+ and Fe,MgOH absorption features,hence the use of different valence state of iron and secondary minerals can distinguish them:ASTER band2/band1 represent Fe3+ distribution,ASTER band2/band1 represent the Fe2+ distribution,RBD6 can estimate the AlOH mineral abundance. Psammitic/pelitic schist containing phengite,chlorite,stilpnomelane,as well as the weathered surface covered by clay minerals,exist characteristic absorption spectrum in the 221 μm(band 6),and has a high reflectance in 165 μm(band 4),while the blueschist/greenschist show high reflectance in the 221 μm(band 6),and it exit low reflectance in 165 μm(band 4),and blueschist/greenschist appear low ASTER band4/band6 ratio.

白云岩的CO2-3吸收谱带中心波长位于232〖KG*3〗μm,与灰岩的CO2-3 吸收谱带中心波长位置235 μm相比,具有向短波长方向移动的特点,据此可以利用RBD7、RBD8分别有效的识别白云岩和灰岩;长英质岩石显示AlOH和Fe3+ VNIRSWIR吸收特征,而基性超基性岩石显示Fe2+和Fe、MgOH特征,利用不同的铁价态和次要矿物可以区分它们:ASTER band2/band1代表了含Fe3+矿物分布信息、ASTER band5/band4代表了含Fe2+矿物分布信息、RBD6可以估计AlOH矿物的丰度;砂质/泥质片岩含较多的多硅白云母、绿泥石、黑硬绿泥石以及风化后表面覆盖的其它粘土矿物,在221 μm(band 6)存在有特征的吸收谱带,并且在165 μm(band 4)具有较高的反射率,而蓝片/绿片岩在221 μm(band 6)反射率较高,不具有明显特征吸收谱带,同时其在165 μm(band 4)反射率较低,因此蓝片/绿片岩ASTER band4/band6 比值低。

During the development peroid of Doushantuo Formation source rocks, the areas studied belong to arenaceous pelitic facies, open platform facies. Until Dengying Stage, the area mainly belongs to restricted platform facies. During early Lower Cambrian, the areas belong to mesa-basin sedimentary facies and gradually developed to open platform-restricted platform facies. During Lower Cambiran, the areas belong to open sea shelf facies-open marine platform facies.

陡山沱组烃源岩发育时期,研究区处于近岸砂泥坪相区及开阔台地相区,至灯影期,主体处于局限台地相带;早寒武世早期,研究区主要处于台地—盆地沉积相带,逐渐演变为开阔台地至局限台地相带;下寒武统在区内以广海陆棚—开阔台地相为主;奥陶纪末—志留纪早期,经历了非补偿滞留还原海盆—正常陆表海/深水陆棚海—残留海—陆相沉积环境的变迁。

Delta plain and delta front subfacies develop sand body, distributary channel, underwater distributary channel and mouth bar are most developed, they are favorable reservoir facies belt in the region of interest.

三角洲平原和前缘亚相砂体发育,其中分流河道、水下分流河道和河口坝砂体最为发育,是研究区有利储层发育相带。

First of all, for the geological features of mud enwrapping sand, seismic features of shallow buried depth, low formation velocity and high resolution of delta front belt, the strong amplitudes of mouth bar sand and underwater distributary channel sand have been clearly recognized with the help of amplitude attribute slice of high-fidelity 3D seismic data along the formation, i.e.

首先针对松辽盆地三角洲前缘相带泥包砂地质特征及埋藏浅、层速度低、分辨率高的地震特征,利用高保真三维地震资料沿层振幅属性切片,有效地识别出了河口坝和水下分流河道砂体的强振幅地震反射特征,即砂岩储层的地震&亮点&特征。

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