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Although there is a little carbonite caused by some magmatic dikes in the CarboniferousPermiam coal, most Carboniferous-Permian coal has no great differences in vitrinite reflectance, crystalline indices, bulk specific gravity, hardness, and the content of velotile matter from the Jurassic coal, and both are super-anthracite.

区内石炭—二叠系煤与侏罗系煤除了前者含有一些由侵入体造成的天然焦或半焦外,二者均为超无烟煤,在镜质体反射率、煤晶核结构、显微硬度、挥发份和容重等方面上均没有明显的差异,说明区域变质是在煤系地层沉积之后发生的。

Two kinds of stable decagonal quasicrystals and 16 approximants have been found in Al-Cr- alloys by means of selected-area electron diffraction, high resolution electron microscopy image and X-ray single crystalline diffraction.

用选区电子衍射和高分辨像等手段,确定了Al-Cr-合金系中的16个准晶近似相,其中的7个准晶近似相为新相,它们是:六方τ相,六方μ′相和正交ε相,以及周期为3.72nm的正交(2/1,2/1),(1/1,3/2),(2/1,3/2)相和α=2.29nm,c=3.71nm,β=108°的单斜相。

TheJiyang depression located in paleomonsoon climate zone in the period of the sahejieformation sedimentation, the wet and hot climate made ancient lake become deeperwater, enhanced stratification, reduced primary productivity of plankton, decreasingsedimentary velocity of carbonate, increasing sedimentary velocity of clay, fortifiedreductibility on certain degree, and then would be available for development of blackshale, dark shale and oil shale; In the contrast, the cold and dry climate lead ancientlake to shallower water, subdued stratification, increaser primary productivity ofplankton, enhancive sedimentary velocity of aphanitic carbonate, decreasedsedimentary velocity of clay, and then would be available for development calciteshale, calcite laminar shale, calcite mudstone, shaly carbonate rock, even laminarcarbonate or dolomite rock.

济阳坳陷在古近系沙河街组沉积期属于古季风气候带,在湿热的气候条件下古湖水加深,分层性增强,浮游生物的古生产力降低,隐晶碳酸盐的沉淀速率变小,粘土沉积速率加快,还原性一定程度上有所加强,有利于黑页岩、油页岩和暗色泥岩的形成:而相对干冷气候下,古湖水变浅,分层性减弱,浮游生物的古生产力增高,隐晶碳酸盐的沉积速率变大,粘土的沉积速率减慢,有利于钙质页岩、钙质纹层页岩、钙质泥岩、泥灰岩甚至纹层状碳酸盐岩、灰岩的发育。

Structure: The structure of Jade variable phenocryst interwoven structure, refers to its metamorphism, the transparent and granular around the porphyroblast small fibrous mineral crystals formed interwoven structure.

结构:翡翠的结构为变斑晶交织结构,系指其在变质作用下,透明粒状斑晶的周围的细小纤维状的矿物晶体交织在一起而形成的结构。

Using the thermodynamic model of TiAl binary system, part of phase diagram of Ti-(44-50)Al around the peritectic reaction was calculated and the solidus and liquidus of primary phase β and peritectic phase α were determined and the parameters used for interface response function were obtained.

利用TiAl二元系的热力学模型,计算了Ti-(44—50)Al合金包晶反应附近的相图,确定了初生相β和包晶相α的固、液相线,得到了界面响应函数所需的部分参数。

The longer fluorinatd alkyl chain on the three-ring was advantageous to the formation of smectic phase. The mesogens with chiral center located between fluorinated tail and mesogenic core exhibited chiral smectic C phase and other smectic phases when the alkoxyl adhering to the other side of the mesogenic core was of intermediate length.

三环系液晶化合物中较长的氟烷基边链有利于近晶相的形成,且当液晶核另一端的烷氧基链的长度适中时,在氟烷基边链和液晶核之间具有手性中心的液晶分子显示了手性近晶C相和其它液晶相。

According to the regression equations of initial crystallization temperature, the solubility of alumina and density at the temperature of 20 ℃ above its ICT of (2.23~3.0)NaF.AlF3-(0~5%)LiF-(0~15%)CaF2 system,the ICT isograms within the range of 910~950℃ and the density isograms at nonequal temperature within the range of 2.04~2.20g/cm3 under the 6%, 8%, 10%solubility of alumina were first obtained respectively.

基于(2.23~3.0)NaF.AlF3-(0~5%)LiF-(0~15%)CaF2系熔体初晶温度、变温氧化铝溶解能力和变温密度的研究,首次得到了氧化铝溶解能力为6%,8%和10%时温度范围在910~950℃的等溶初晶温度和密度在2.04~2.20g/cm3之间的等溶变温密度。

Common rolling plank is shown intense (orientaton of 0002) tool reference plane, after rolling of horn waiting for diameter, plank grain orientaton by original (change of orientaton of 0002) tool reference plane is; of orientaton of blame tool reference plane the existence after strain crack of common rolling plank is many twin brilliant, amount of brilliant of twin of drawing of direction of rolling of edge of plank of rolling of horn w

普通轧制板材呈强烈的(0002)基面取向,等径角轧制后,板材晶粒取向由原来的(0002)基面取向转变为非基面取向;普通轧制板材拉伸断裂后存在大量孪晶,等径角轧制板材沿轧制方向拉伸孪晶数量明显减少,等径角轧制有可能启动了新的滑移系,而拉伸孪生只是作为一种协调变形机制。

The vapor phase deposition, axial screw dislocation and surface diffusion play important roles in the whisker growth.

在大量的Bi系晶须生长实验的基础上,本文提出了晶须生长的机理,气相沉积,轴向螺位错和界面扩散在晶须生长过程中起了重要作用。

Different from the perieutectic reaction Liq+δ→β, perieutectic reaction in Al-Si alloys containing Mn acts as Liq+δ→α.

与铝硅铁三元系中的包晶反应Liq+δ→β不同,加锰铝硅合金中δ铁相的包晶反应则以Liq+δ→α的形式进行。

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