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The phylogeny tree indicated that Tibet goat, ChengDugoat, JinTang black goat and Beichuan white goat formed a branch, and LeZhi black goat andJianChang black goat formed a branch, and the next was Jian Yang daer goat.

以Nei's遗传距离为基础构建的系统发生树表明,藏山羊和金堂黑山羊、成都麻羊、北川白山羊聚为一类,乐至黑山羊和建昌黑山羊聚为一类,而简阳大耳羊自成一类。

Dielectric layer patterns which define recesses in which damascene interconnections are to be formed, are formed.

形成限定凹槽的介电层图形,在该凹槽中将形成镶嵌互连。

Results :①The MVs were formed by osteoblast of the secret type、dentinoblast and process;② There was a mature process of the MVs in the extracellular matrix.The appearance of the hydroxyapatite was a major mature feature;③ HAP formed initially in the MVs entered into collage matrix and eventually mineralized;④ The shifting sign of HAP from MVs to the surface of collage fibril was observed.

结果:①MVs是由分泌型成骨细胞、成牙本质细胞及其突起芽生进入胶原基质;②MVs在细胞外胶原基质中有一个逐渐成熟的过程,并以羟基磷灰石(hydroxyapatite,HAP)晶体的出现为其主要特征;③HAP在MVs内形成、增多,最终进入胶原基质并进一步沉积、钙化;④部分胶原原纤维表面沉积的HAP 晶体与MVs分泌的晶体有明显的移形迹象。

In the passivated REBAR electrode surface formed by ORCs the grain observed from AFM examination is composed of γ-Fe〓O〓 and Fe〓O〓 0 At+0.7V, the passive film on REBAR electrode formed by single-step polarization is composed of Fe (Ⅲ oxide highly doped by Fe〓. In some areas, small γ-Fe〓O〓 particals or some polymeric structure which contains dioxy and dihydroxy bridging bonds between the iron atoms may also exist in the other region.

通过AFM实验观察到的钢筋电极经循环电位扫描至+0.7V形成的钝化膜中具有的结晶颗粒主要由γ-Fe〓O〓和Fe〓O〓·yH〓O0 阶跃电位形成的钢筋钝化膜在+0.7V下主要是由掺杂了大量Fe〓的三价铁氧化物构成,在某些微小的区域可能存在γ-Fe〓O〓微晶,而在另外一些区域则具有聚合物膜的结构。

The characteristics of elements shows that magma of fine dioritequartz diorites derived from the enriched mantle or lower crust undergone ocean crust subducting and dehydrating, and was formed and emplaced in the process of crust growth. The magma of dioritic porphyritedacitic porphyries emplaced relatively late, it might derive from upper crust or undergo intensive contamination of crustal materials, and was formed in the proces of crust thining. These characteristics suggest that the geodynamics background of the Jinchanggouliang gold deposit formation is the transition process from compression to extension.

元素地球化学特征显示:细晶闪长岩-石英闪长岩的岩浆源于富集地幔或洋壳俯冲脱水交代的下地壳,地壳增厚过程产生并就位;闪长玢岩-英安斑岩类的岩浆就位相对晚,来源具有上地壳性质或被地壳物质强烈混染,地壳减薄过程形成;这种特征暗示金厂沟梁金矿形成的地球动力学背景是在地壳挤压增厚转化为伸展减薄过程。

CuS and CdS nano-particulate films were obtained with these two methods, and some interesting phenomena were observed: under the Gibbs film formed by CTAB, CuS nano-rods were obtained at the oil/water interface, and disklike aggregates of CdS nano-crystals were obtained at both the air/water and oil/water interfaces; under the Langmuir film formed by NaAOT at air/water interface, disk-like aggregates of CdS were also obtained.

利用此两种反应技术,制备了CuS和CdS颗粒膜,并研究了它们的一些光电性质;在Gibbs膜下,得到了棒状CuS纳米晶。由发现的表面活性剂形成的带状物,提出棒状CuS晶体是以带状聚集体为模板形成的;在液-液、气-液界面Gibbs膜下反应中,发现CdS纳米颗粒的盘状聚集体的形成,这是由于表面活性剂在界面上形成的二维胶束而造成的;在气-液界面上Langmuir下的反应中,也发现CdS盘状晶体的生成。

Snow dooms were formed in middle of water where rocks should be seen in summer; and thin ice formed on shallow water.

雪包在水的中央形成各种形状,柔化了下面的岩石。水浅的地方,已经有一层薄薄的冰。

On a mirror surface, after performing coloring process in the stainless coloring solution containing CrO3 and H2SO4, drawbench or matt stainless steel board/foil as thick as 0.01 to 3 mm images the deadee by printing or photosensitivity, so a middle protection film is formed on the stainless steel surface; then by processing stripping, the archaized deadee is formed on the stainless steel.

本发明涉及一种不锈钢仿古遗像制作方法,在厚度0.01~3mm的镜面、拉丝或哑光不锈钢板/箔,通过在含CrO 3 和H 2 SO 4 的不锈钢着色溶液中着色处理,把遗像通过印刷或感光成像,在不锈钢表面上形成遗像中间保护膜;再进行去膜处理,在不锈钢上形成仿古遗像。

In Modular Organization, associated boundary which is formed in the base of relationship network replaces entitative boundary which is formed in the base of administrative order.

首先,识别并界定了模块化组织边界,认为模块化组织边界是指依据模块化组织基本架构和主导规则所建立起来的关系网络的界限范畴。

The hypo-volcanic crytoexplosion Breccia rock body is formed of granite magma, which is rise to the lower of the earth s crust along the east-western shear zone and exploded below the Archean fundus rock. The felstone vein and the hypo-volcanic crytoexplosion Breccia rock are from the same magma source, and are formed in the different evolution stages.

香炉碗子金矿区分布的次火山隐爆角砾岩体是由花岗质岩浆沿东西向脆~韧性剪切带上升到地壳浅部隐爆太古代基底岩石所形成,霏细岩脉与次火山隐爆角砾岩来自同一岩浆源,为同一岩浆活动不同演化阶段所形成的。

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