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The intermediate-basic volcanic rocks with SiO2 content less than 57.48 wt% are high in Al2O3(20.22-16.34 wt%) and K2O, enriched in large ion lithophile elements, show obvious Nb, Ta negative anomaly, these are same to the basalts which formed in island arc. The andesite, dacite and rhyolite rocks with SiO2 content between 62.11-75.19 wt%, are similar with the I-type granitic rocks formed in island arc in their geochemistry. It is suggested that the Jueluotage area of East Tianshan was in island arc setting during Late Carboniferous, when the subduction of the ancient Asian Ocean was in progress.

其中w(SiO2)小于57.48%的中基性火山岩具有高w(Al2O3)(16.34%~20.22%),较富钾,富集大离子亲石元素,具明显的Nb、Ta负异常;w(SiO2)介于62.11%~75.19%之间的安山岩、英安岩和流纹岩岩石化学特征与准铝质的Ⅰ型花岗质岩石相似,其地球化学特征也反映出岛弧花岗岩的特点,表明东天山觉罗塔格地区路白山一带在晚石炭世仍处于古亚洲洋向南俯冲的岛弧环境。

You will come in May between June, between choice section shorter give birth to half lignification branch in those days, from base the ministry cuts dirty to insert spic, topmost reservation comes 3 pieces 5 flocculus, if branch is too long, yi Ke bite off carries a tip on the head, cuttage medium can use humus soil of orchid mud, high mountain, vermiculite, pearlite or Huang Xin earth to wait, thick about 15 centimeters reach 20 centimeters, the catchment layer that lower berth reachs 8 centimeters 7 centimeters; medium after in season is wet, in will inserting spic to insert matrix, deepness of the be buried that insert spic makes an appointment with the 1/2 that grows for spic, a few cuttage also can choose the family full-dress medium generation makes big flowerpot cuttage seedbed.

你可于5月至6月间,选择节间较短的当年生半木质化枝条,自基部切下作插穗,顶端保留3片至5片小叶,若枝条过长,亦可截去顶梢,扦插介质可用兰花泥。高山腐殖土。蛭石。珍珠岩或黄心土等,厚约15厘米至20厘米,下铺7厘米至8厘米的排水层;把介质喷湿后,将插穗插入基质中,插穗入土深度约为穗长的1/2,家庭少量扦插也可选用大花盆盛装介质代作扦插苗床。插后加盖塑料薄膜保湿,温度控制在25℃至30℃之间,加设荫棚遮挡阳光,或挪放于树荫下,始终保持扦插基质湿润,东鹃约过1个月即可生根,而西鹃则要60天至70天才能生根。9月后可减少遮荫时间,并追施稀薄尿素液一次,浓度约为0.2%,10月下旬即可上盆。

Geek in the pink Well let the geek in the pink take a stab at it If you like the way I'm thinkin' baby wink at it I may be skinny at times but I'm fat fulla rhymes Pass me the mic and I'm a grab at it well isn't it delicious crazy way that I'm kissin' Cause baby listen to this don't wanna miss it while it's hittin' Sometimes you gotta fit in to get in But don't ever quit cause soon I'm gonna let you in but see I don't care what you might think about me You'll get by without me if you want I could be the one to take you home Baby we could rock the night alone If we never get down it wouldn't be a let down But sugar don't forget what you already know I could be the one to turn you out We could be the talk across the town Don't judge it by the color, confuse it for another You might regret what you let slip away Like the geek in the pink pink pink Like the geek in the pink yeah Well this relationship fodder don't mean to bother nobody But Cupid's automatic musta fired multiple shots at her Because she fall in love too often that's whats the matter At least I talk about it keep a pattern of flattery and She was starin' through the doorframe and eyeing me down like already a bad boyfriend Well she can get her toys outta the drawer then Cause I ain't comin' home I don't need that attention, see I don't care what she might think about me she'll get by without me if she want I could be the one to take her home Baby we could rock the night alone If we never get down it wouldn't be a let down But sugar don't forget what you already know I could be the one to turn you out We could be the talk across the town Don't judge it by the color, confuse it for another You might regret what you let slip away Hey baby look at me go From zero to hero You better take it from a geek like me I can save you from unoriginal dum-dums Who wouldn't care if you com...plete him or not So what I've got a short attention span A coke in my hand Because I'd rather have the afternoon, relax and understand My hip hop and flip-flops well it don't stop with the light rock A shot to mock you kinda puts me in the tight spot The hype is nothing more than hoo-ha so I'm Developing a language and I'm callin' it my own So take a peek into the speaker and you'll see what I mean That on the other side the grass is greener I don't care what you might think about me You'll get by without me if you want I could be the one to take you home Baby we could rock the night alone If we never get down it wouldn't be a let down But sugar don't forget what you already know I could be the one to turn you out We could be the talk across the town Don't judge it by the color, confuse it for another You might regret what you let slip away

怪胎的粉红色那么让怪胎的粉红色就在它刺伤如果你喜欢的方式我thinkin '婴儿在这眨眼我可能有时瘦,但我胖fulla韵我的通行证麦克风和我是一个抓住它以及是不是疯了美味的方式,我基辛'原因婴儿收听此不想错过它,而它的hittin '有时候,你总得适应进入但是,不要任何时候都很快退出事业我一定让你看到的,但我不在乎你们可能认为我你会得到的没有我如果你想我可以是一个带您回家宝贝我们可以岩夜间单独如果我们永远不会下跌不会是一个放下但是,糖不要忘记你已经知道我可以是一个把你我们可以谈论整个镇不要判断它的颜色,它混淆另一你可能会感到遗憾的是你让溜走像怪胎的粉红粉红粉红像怪胎在粉红色的是那么这种关系的饲料并不意味着没有人打扰但丘比特的自动穆斯塔发射多种拍摄她因为她爱上往往是什么问题至少我谈论这件事保持一贯奉承和她starin '通过门框和关注我已经想了一个坏男友那么她可以让她的玩具outta然后抽屉原因我不是comin家里我不需要注意,见我不在乎什么,她可能认为我她会没有我的,如果她想我可以是一个带她回家宝贝我们可以岩夜间单独如果我们永远不会下跌不会是一个放下但是,糖不要忘记你已经知道我可以是一个把你我们可以谈论整个镇不要判断它的颜色,它混淆另一你可能会感到遗憾的是你让溜走喂婴儿看我走从零到英雄您是否可以更好地从一个像我这样的怪胎我可以为您节省来自非独创的达姆, dums 谁不会关心你的COM 。。。他完全或不所以我有一个短期注意跨度焦炭在我的手因为我宁愿有下午,放松和理解我的嘻哈和触发器以及它不停止与轻摇滚一杆嘲笑你有点儿让我在紧张的现场宣传只不过是豪哈所以我开发的一种语言,我callin '但我自己因此,需要看到的发言,你会明白我的意思这在另一边的草绿色我不在乎你们可能认为我你会得到的没有我如果你想我可以是一个带您回家宝贝我们可以岩夜间单独如果我们永远不会下跌不会是一个放下但是,糖不要忘记你已经知道我可以是一个把你我们可以谈论整个镇不要判断它的颜色,它混淆另一你可能会感到遗憾的是你让溜走

According to petrographic facies test, gravel sample mainly consists of quartz, albite, dolomite, and minor biotite; and sand sample is mainly made up of quartz and albite. As an important ASR active mineral, chalcedonite exists in fractures of dolomite and in matrix of cherty limestone. In rapid mortar bar test, expansion of sand, small gravel and middle gravel at 14 day are less than 0.1%, but keep increasing in long term.

岩相法检测显示卵石样品主要由石英、钠长石及白云石和少量云母类矿物组成,砂样品主要由石英、钠长石等矿物组成,重要的碱活性物质玉髓主要出现在白云岩裂隙和硅质灰岩的基质中;&砂浆棒快速法&检测结果显示砂、小石、中石样品14天的膨胀率均不超过0.1%,为非碱-硅酸反应活性骨料,但卵石样品仍具有一定的碱活性,且后期膨胀率一直持续增长。

The influential factors are: horizon, different system in strata sequence framework, clast composition, structure, matrix quality in source area, sedimentary facies belt, diagenesis, volcanics distribution and pressure distribution.

储层物性的影响因素主要有:层位、层序格架内不同体系域、碎屑组份、结构及物源区母岩性质、沉积相带、成岩作用、中基性火山岩分布、压力分布等。

There are 4 end members of volcanic clasts, including catapult airfall, ejection airfall, base surge and volcanic clasts flow.

与火山作用有关岩相有4种端元的火山碎屑岩相:弹射坠落爆发空落相、喷射降落爆发空落相、热碎屑流相和热基浪相。

If the volcanic clasts were deposited on volcanic slope and/or fluvial plain, they would occur in the 4 faceis mentioned above or in alluvial fan and braid stream.

与火山作用有关岩相有4种端元的火山碎屑岩相:弹射坠落爆发空落相、喷射降落爆发空落相、热碎屑流相和热基浪相。

The exposed massive cold-seep carbonates provided substrate for the encrustations of corals as well as coralline algae and might have played a crucial role in the initial development of coral reefs in a siliciclastic paleoenvironment of active tectonic setting. This is probable the first case of the world that cold-seep carbonates acting as initial colonization hardgrounds of hermatypic corals and corallines.

在此基底泥岩快速浅化的过程中,出露的块状冷泉碳酸盐岩成为不稳定地体构造背景中,珊瑚与珊瑚藻等表覆生物在矽质碎屑环境生长的硬底质,可能在礁体的最初发育扮演关键性的角色;此种冷泉碳酸盐岩成为造礁珊瑚与珊瑚藻在矽质碎屑古环境中最初生长硬底质的现象,很可能为世界首例。

The stratum of the area is proterozoic,Tao wan group(Pt1t).The nephrite deposit wasformed in carbonate rocks or calcium mudstones of shallow-sea facies, which was penetratedby basic magmatic rocks, Jinningian gabbro .

该区地层为下元古界桃湾群(Pt1t),玉矿赋存于浅海相泥质碳酸盐岩及钙质泥岩,局部夹中基性火山岩的桃湾组中。

The data show the following ages: 1894±17 Ma and 1847±59 Ma for garnet pyroxenite of the Tiantangshan Group complex, indicating a Paleoproterozoic age; 1462±28 Ma for the metabasic volcanic rocks of the Yunkai Group complex, indicating the presence of fragments of the Meso- and Neoproterozoic oceanic crust in the Yunkai area; 906±24 Ma for the granitic gneiss intrusion is, which should be the product of the global Grenville collisional orogeny occurring around 1000 Ma BP. In addition, an inherited detrital zircon age of 2702±13 Ma was also obtained, which is the oldest age in the Yunkai area and even in Cathaysia, proving the presence of Neoarchean continental crustal material in Cathaysia.

获得天堂山岩群石榴辉石岩的形成年龄为1894Ma±17Ma和1847Ma±59Ma,表明其时代为古元古代;云开岩群洋中脊型变质基性火山岩的喷发年龄为1462Ma±28Ma,证明该地区存在中元古代的古洋壳残片;获得花岗质片麻岩的侵入年龄为906Ma±24Ma,应为1000Ma前后发生的全球性Grenville期造山作用的产物,并获得2702Ma±13Ma的继承碎屑锆石年龄,这是云开地区乃至华夏古陆目前获得的最古老年龄,证明华夏古陆曾存在新太古代陆壳物质。

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