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According to mineral components, ores of the Daixian rutile deposit can be classified into the following types: actinolite- bearing anthothyllitite, actinolite-garnet- bearing anthothyllitite, staurolite- actinolite- bearing anthothyllitite, actinolite-biotite-bearing anthothyllitite, kyanite-bearing anthothyllitite, talc-actinolite- bearing anthothyllitite and chlorite-actinolite-bearing anthothyllitite, etc.

山西代县金红石矿床的含矿岩石按岩石中矿物组成可以划分以下几种类型:阳起直闪岩、直闪阳起直闪岩、石榴石阳起直闪岩、十字石阳起直闪岩、阳起黑云直闪岩、阳起直闪岩、蓝晶石直闪岩、滑石阳起直闪岩、绿泥阳起直闪岩等。按金红石的颜色可以划分为两类,即红色金红石矿石、黑色金红石矿石。

This study is to give a solution for the estimation of flash point for mixtures, the necessity for classification of flammable liquids. The traditional models for predicting flash point of mixtures usually by the activity coefficient approach. However, the parameters of activity coefficient were regressed from phase equilibrium data in the literatures. If there is no such parameter in literatures for the desired mixture, the model cannot predict the flash point oft hat mixture. Thus, this research aims at the improvement of deficiency of the flash point prediction models in the literatures by useing UNIFAC (Universal Quasi-chemical Functional Group Activity Coefficient) equation, Dortmund-UNIFAC equation and Lyngby-UNIFAC equation. In this study, we were aim at the prediction model for miscible mixtures.From the result, it is suggested to use different type of UNIFAC equation to estimast activivity coefficient in the predition of flash point for different mixture type.

易燃液体分类的主要依据参数为闪火点值,因此本研究目的为解决易燃液体中混合物分类时所面临到的闪火点值缺乏的问题,而在过去文献中所提出的闪火点预测模式会使用到活性系数,但这些模式使用到的活性系数均需要相平衡的数据以回归其所需参数,若所欲估算闪火点的混合溶液文献上未有相关参数,则无法有效利用闪火点预测模式估算其闪火点,因此针对文献中现有闪火点预测模式的缺点,利用描述液体混合物活性系数UNIFAC (Universal Quasi-chemical Functional Group Activity Coefficient)方程式、Dortmund-UNIFAC方程式和 Lyngby-UNIFAC方程式,建立发展一闪火点预测模式,而本研究以互溶溶液为对象。

Taiwan drove to the 21 line continued to visit on the 12th bridge, the entrance to a note card, that is, at the entrance to Mount Zion, according to indicators continued to turn left can see the door of Zion Holy Mountain, above the two white A winged cherubim (Mount Zion built cherubim door is symbolic of God Chapai angel guards the road leading to the tree of life, security guards God's sacred mountain, symbol of human life to the Eden tree has smooth the road), The mood is extremely beautiful; along the way can also see many of special significance to the beautiful scenery and attractions, such as the Tianchi Zion, David Castle, the Arc de Triomphe House, Victory Tower, the Monument of truth over power, Tianxiayijia, Meiyuan, Ting Li-jun, The altar, the Temple of Christ is the rock, flashing the tent, Zion tree house, and so on the beautiful scenery, as if your exposure in the nature of worldly paradise!

驱车前往台21线续行至12号桥头处,可以入口处有一说明牌,此即为锡安山的入口处;依指标左转续行可以看见锡安圣山的大门,上面安有两个白色著翅膀的基路伯(锡安山建基路伯大门乃象征神差派天使看守通往生命树的道路,护卫神的圣山,又象征人类通往伊甸生命树的道路已经畅通了),意境极为优美;沿途也可以看见许多具有特殊意义的景物和美丽的景点,如锡安天池、大卫城堡、凯旋楼、胜利大楼、真理战胜强权纪念碑、天下一家、梅园、立君亭、祭坛、圣殿、基督是磐石、闪的帐棚、锡安树屋等等美丽的景致,让您置身在彷佛人间仙境的大自然中!

The Akkadians were Semites, that is, they spoke a language drawn from a family of languages called Semitic languages (the term "Semite" is a modern designation taken from the Hebrew Scriptures; Shem was a son of Noah and the nations descended from Shem are the Semites).

阿卡德人是闪族,他们说的语言是出自一个被叫闪族语系的语种(闪族的这个词的现代名称来源于希伯莱语的文稿/旧约经文,闪是诺亚的一个儿子,由闪而来的民族,便被叫做闪族)。

The Indosinian granitoid belt in South Qinling, Central China, is lithologically composed of diorite, monzodiorite, tonalite, granodiorite and granite, as well as widely distributed mafic microgranular enclaves and dykes within the intrusions.

南秦岭印支期花岗岩带的岩石组合包括闪长岩、二长闪长岩、英云闪长岩、花岗闪长岩和花岗岩等,岩体内广泛存在镁铁质微粒包体和脉体。

Neoproterozoic Baoxing Complex in middle to lower metamorphic grade, located in western margin of Yangtze Craton, consists mainly of metamorphic gabbroic, dioritic gneisses, tonalitic and granodioritic gneisses, and massive monzogranites The studies of petrochemistry and SmNd isotopes of Baoxing Complex reveal that the gabbroic and dioritic magmas came from a congenetic magma derived from the partial melting of spinel lherzolites in depletive mantle, and that the magma was intensively contaminated by crustal materials during its emplacement The tonalitic and granodioritic magma were derived from the partial melting of metamorphic basalts in the lower crust And the monzogranitic magma was formed from partial melting of metagreywacks Integrating the lithological association, their trace elements, SmNd isotopic characteristics and petrogenesis, the Baoxing Complex must likely have been emplaced in an island arc tectonic background at the Neoproterozoic active continental margin of Yangtze Craton

位于扬子克拉通西缘的新元古代宝兴杂岩主要由中低级变质的辉长质片麻岩、闪长质片麻岩、英云闪长质到花岗闪长质片麻岩和块状二长花岗岩组成。岩石地球化学和SmNd同位素特征表明,辉长质片麻岩和闪长质片麻岩为同源岩浆演化序列,原始岩浆起源于亏损地幔尖晶石橄榄岩的部分熔融,在上升和侵位过程中受到了地壳岩石强烈混染。英云闪长质和花岗闪长质岩浆形成于下地壳玄武质岩石部分熔融,而二长花岗质岩浆形成于杂砂岩的部分熔融。综合分析宝兴杂岩的岩石组合、微量元素和同位素特征,该杂岩体最有可能形成于新元古代活动大陆边缘火山弧构造背景,并可能经历了碰撞过程。

Detailed geology- petrology-mineralogy study shows that late Triassic-early Jurassic granites can be divided into 4 groups: granodiorites, monzonitic-K syenogranites mainly, alkali feldspar-alkali granites and syenite, Middle Jurassic granites is composed of quartz diorites-granodiorites and monzonitic granites, the main rock type includes granodiorites and monzogranites; Early Cretaceous granites include alkali gabbro, alkali granites and granodiorites, and these rocks composed bimodal igneous rock group.

详细的地质-岩石矿物学研究表明,晚三叠-早侏罗世花岗岩可以划分成四种岩石组合,即花岗闪长岩组合、二长花岗岩—正长花岗岩组合、碱长花岗岩—碱性花岗岩组合和正长岩组合,其中以二长花岗岩—正长花岗岩组合为主;中侏罗世花岗岩由石英闪长岩-花岗闪长岩组合和二长花岗岩组合构成,岩石类型以花岗闪长岩和二长花岗岩为主;早白垩世出现了碱性辉长岩、碱性花岗岩和花岗闪长岩,构成双峰式火成岩组合。

Based on isotopic ages and the cycle of magamtism, the ages of Yanbian granites can be subdivided into five periods:①late Permian granites (260-245Ma), the typical plutons are Liukesong and Liangbing plutons, and the main rock type include diorite-monzonitic-K syenogranites;②Triassic granites (225-200Ma), the typical plutons are Sandaogou, Chunyang, Qishiergedingzi, Dahuanggou, Naozhi, and Qinglinzi plutons, the main rock type include quartz dioritesgranodiorites-monzonitic-alkali granites;③early Jurassic granites (190-180Ma), which composed of quartz diorites-granodiorites - monzonitic ,and the typical plutons are Shimen, Miantian, Daxinggou and Yushuchuan rock;④Middle-Late Jurassic (170-150Ma), which composed of granodiorites- monzonitic- garnet-bearing muscovite granites, the typical plutons are Huangniling, Weizigou, Loutuoshan and Dongqing rock;⑤early Cretaceous (about 130Ma), the typical pluton is Zhongping pluton, and its rock type is paulite diorite.

另外,根据同位素年龄和岩石组合并考虑到岩浆的旋回性,将延边显生宙花岗岩进一步划分为五个期次:1。晚二叠世(260-245Ma),代表性岩体为六棵松和亮兵,主体岩性为辉石闪长岩、二长花岗岩和钾长花岗岩;2。三叠世(225-200Ma),代表性岩体为三道沟、春阳、七十二个顶子、大荒沟、闹枝、青林子,岩石组合为石英闪长岩—花岗闪长岩—二长花岗岩—碱长花岗岩,以花岗闪长岩和二长花岗岩为主;3。早侏罗世(190-180Ma),石英闪长岩—花岗闪长岩—二长花岗岩组合,主体岩性为花岗闪长岩,代表性岩体有石门、棉田、大兴沟、榆树川等;4。中侏罗世(170-150Ma),主体岩性为花岗闪长岩和含石榴石花岗岩,代表性岩体有黄泥岭、苇子沟、骆驼山、东清5。

Up above the world so high, Like a diamond in the sky. When the blazing sun is set, And the grass with dew is wet, Then you show your little light, Twinkle,twinkle,all night. Then the traveller in the dark, Thanks you for your tiny spark; He could not see where to go If you did not twinkle so. In the dark blue sky you keep, And often through my curtains peep, For you never shut your eye Till the sun is in the sky. As your bright and tiny spark Lights the traveller in the dark, Though I know not what you are, Twinkle ,twinkle,little star.

泰勒 一闪一闪,小星星你是什么,我弄不清大地之上高高挂好似钻石缀天空当炽热的太阳落西方露水将芳草浸湿时天庭之上你放微光一闪一闪彻夜亮暗夜茫茫行者难多亏这微光把路牵如你不曾频闪光行者怎能辨方向守在天庭深邃邃的蓝透过窗帘你常偷看因你从不歇歇眼直到太阳升天边你的光芒轻且亮给暗夜的行者指方向虽然你是什么我弄不清一闪一闪,你这小星星。

He remarked that the Flora of Massachusetts embraced almost all the important plants of America, most of the oaks, most of the willows, the best pines, the ash, the maple, the beech, the nuts.

他经常使用的武器之一,这个比一般调查者显微镜和酒精里的标本更重要,就是他一闪的灵光,这生长自他长期以来的勤奋,但却是以最严肃的论述出现,名义上是对自己的家乡和邻居的讴歌,认为那是他最喜欢的观察自然的场所。

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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。

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