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花岗岩

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The kitchen offers integrated appliances such as a dishwasher, washer/dryer, fridge, microwave and hob and is finished to a very high standard with cream granite worktops and marble tilling.

厨房设施齐全,有洗碗机、冰箱、微波炉、烤架,奶油色高品质花岗岩台面,大理石橱柜。

Fully fitted kitchen including granite worktop, extractor fan unit, built-in oven and hob.

充分配备厨房,包括花岗岩worktop ,萃取范单位,内置在烤箱和滚刀。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究,精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现,把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带;初步确定该区的变质作用属于中温-低压型,变质作用发生的时代为290Ma左右,是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原&居里得能组&岩屑砂岩的碎屑锆石SHRIMP U-Pb定年,确认这套地层的沉积不早于晚泥盆世,很可能是石炭纪,而不是前人所说的前寒武纪;结合对其区域地质背景、源区位置和沉积环境分析,推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料,结合该区已有相关资料的综合研究,确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪,不存在泥盆纪的岩浆岩,进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料,把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%,相应的地壳缩短量分别为4.3km、9km和11.3km。

The central peaks of several craters on the flanks of Syrtis Major are made up of an even more silica-rich rock, granite, that may have formed by extreme crystal separation or by large-scale remelting of earlier basalts.

在大三角侧面,几个火山口的中间尖点是由一种矽含量更高的岩石──花岗岩所构成,可能是经极度晶体分化,或早期玄武岩大范围重新熔融而形成。

The verticality of rim and web Granite table, V block, square, Filler guage

筋板面板的垂直度(花岗岩平台, V 型铁,直角尺,塞尺

All of the studies in this paper, including the study of leaching behavoirs of HLW glass under repository conditions, low oxgen and multi-barrier media; the geochemical model PHREEQC used for calculating the leachate compositions and sediment phases on the glass surface; A Monte Carlo model established and used for study of leaching behavior of HLW-glass; as well as the high-temperature self-propagating synthesis used for immobilization of Sr element in perovskite synroc, are the front research works of this field in the world, and obtained some significative results in theory and practice.

本研究所作的高放废液玻璃固化体在模拟地质处置条件下(低氧条件和多种地质介质)的浸出行为研究,采用了低氧条件和多种模拟地质介质,包括北山预选厂址的花岗岩、膨润土、水泥和Fe〓O〓作为浸出介质,模拟地下水和去离子水作为浸出剂,90℃和150℃两种浸出温度;采用了地球化学模型PHREEQC(version2.7)研究玻璃固化体浸出液中主要元素的浓度以及沉积相的生成;采用蒙特卡罗法建立玻璃固化体的计算模型,对玻璃固化体的浸出行为进行研究;采用了自蔓延高温法固化锶,这些工作都是当前国际上比较前沿的研究课题,采用了先进的分析测试技术,并且作了大量计算,得出了理论上和实践上有意义的结果。

By studying the deformation and evolutionary sequences around the Panshan granitic pluton, east-central Yanshan orogenic belt, and 40 Ar/ 39 Ar thermochronological test and analysis,we present the structural evolutionary process of the overlying strata before pluton intruded as well as it was intruding. The sequences of regional deformation are as follows: before the intrusion of Panshan granitic pluton, the N-S trend contraction in the east-central Yanshan orogenic belt took place, which resulted in the regional EW-trending Malanyu multi-fold and Jixian thrust fault; then Panshan granitic pluton intruded into the south limb of the Malanyu multi-fold and cut-through the Jixian thrust fault; later, the reactivity of the Jixian thrust fault cut off the synclines around thePans han granitic pluton.

通过对燕山东段盘山花岗岩岩体周缘构造变形特征、演化过程的研究,并结合40Ar/39Ar 热年代学测试和分析,提出盘山岩体侵位前、侵位时其上覆岩层的构造演化过程:三叠纪末(210-200 Ma)盘山岩体侵位前,燕山中东段受南北向挤压作用形成了近东西向的马兰峪复背斜和蓟县逆冲断裂;盘山岩体侵位于先期形成的马兰峪复背斜南翼,并侵蚀了蓟县断裂;蓟县断裂的后期再次活动截切了盘山岩体的周缘向斜。

The Mazhashan syenites in the Bachu area were formed in the Late Permian with the zircon SHRIMP age ranging from 286 to 277Ma, and these ages are consistent with the ages (300-260 Ma) of the post-collisional granites in the southern Tianshan orogen.

巴楚麻扎山正长岩体形成于286~277 Ma,属于晚二叠世,与南天山造山带晚二叠世花岗岩(300~260 Ma)相一致。

With the home cook in mind, Johnny offers tips on simplifying professional recipes and provides basic recipes for transcendent cakes, cookies, tuiles, ice creams, sorbets, granités, and more.

同民政库克有鉴于此,约翰尼提供提示简化专业食谱,并提供基本配方超越蛋糕,饼干, tuiles ,冰淇淋,果子露,花岗岩等。

The research of the ore-bearing symptoms of granite , that have contract with minerals ,can offer new method and idea in geology exploration in Eastern Tianshan.

对与该区矿产有密切成因联系的花岗岩含矿性的研究,有助于为东天山的地质找矿工作提供新思路和新方法,并为东天山地区铜、金成矿模式的研究,提供理论依据。

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Do you know, i need you to come back

你知道吗,我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书,王祥生,李德昌。安徽省首次发现嗜群血蜱。

Chapter Three: Type classification of DE structure in Sino-Tibetan languages.

第三章汉藏语&的&字结构的类型划分。