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The measurements used are fork length, head length, upper jaw length, snout length, length of dorsal fin base and anal fin base and the distances from the tip of snout to insertion of dorsal fin, to pectoral fin, to ventral fin and to hard margin of preopercle.

此所用於分析之外部非体节形质计有:尾叉、头、上颚、吻、眼径、背鳍基底、臀鳍基底以及吻端到前鳃盖骨后绿、背鳍起点、腹鳍起点、臀鳍起点等11个形质。

This rock zone, with a NE striking, the whole length of 1 400 km and the width of 100~150 km, is characterized by not onlyalkaline rocks (analcite biotite olivine melilitites, leucititic alnoites, nephelite syenites, aegirite augite syenites, melanite syenites, riebeckite syenite and aegirite bearing quartz syenites) and alkaline granite (riebeckite granite, and aegitite augite riebeckite granite), but also a lot of syenites, monzonites and alkaline feldspar granites or miarolitic K feldspar granites.

该岩带全约1400km,宽100~150km,不仅发育有狭义的碱性岩(方沸黑云橄榄黄岩、白榴黄煌斑岩、霞石正岩、霓辉石正岩、黑榴石正岩和含霓石石英正岩)和碱性花岗岩(钠闪石花岗岩、霓辉石钠闪石花岗岩),还发育有大量的正岩类二岩类碱花岗岩或晶洞钾花岗岩。

Beautiful Ting grows Yu Xie normally, grow 35 ~ 100cm; Raceme grows 25 ~ 40cm, have most flower, 8 bunch give birth to 3 ~ at luxurianting an armpit inside; Bud piece small, bristle shape; Perianth piece quadrature circle or rules round form wrap around needle form, long make an appointment with 3.5mm, purple; Filament is long make an appointment with 1.5mm; Antheral grow 1.5 ~ 2mm; Ovary is close globose, style is long make an appointment with 2mm, post 3 crack.

花葶通常于叶,35~100cm;总状花序25~40cm,具多数花,3~8朵簇生于苞片腋内;苞片小,刚毛状;花被片矩圆形或矩圆状披针形,约3.5mm,紫色;花丝约1.5mm;花药1.5~2mm;子房近球形,花柱约2mm,柱头三裂。

Journey 歌手:张韶涵专辑:over the rainbow 曲:corrinne may 词:corrinne may it's a long long journey till i know where i'm supposed to be it's a long long journey i don't know if i can believe when shadows fall and block my eyes i am lost and know that i must hide it's a long long journey till i find my way home to you many days i've spent drifting on through empty shores wondering what's my purpose wondering how to make me strong i know i will falter i know i will cry i know you'll be standing by my side it's a long long journey and i need to be close to you sometimes it feels no one understands i don't even know why i do the things i do when pride builds me up till i can't see my soul will you break down these walls and pull me through cause it's a long long journey till i feel that i am worth the price you paid for me on calvary beneath those stormy skies when satan mocks and friends turn to foes it feel like everything is out to make me lose control coze it's a long long journey till i find my way home to you..

to you 这是一段很的旅程直到我明白那里是我认为的去处这是一段很的旅程而我不知道是否能相信当阴影落下阻挡了我的视线我失败了并且明白我必须躲藏这是一段很的旅程直到我找到回家的路是走向你我曾用尽了许多日子来回漂流在无人的岸边疑惑著我的目的是什么疑惑著如何使自己更坚强我知道我将会变的脆弱我将会哭泣我知道你将会站在我的身边这是一段很的旅程而我需要更向你靠近有时候这种感觉没有人能了解我不曾知道为何我完成了那件做过的事当骄傲像高墙般将我拱起直到我看不到自己的灵魂你是否会拉著我穿越过这高墙因为这是一段很的旅程直到我觉得那代价是值得的你给了我基督受难像在这暴风雪的影响下当人们魔鬼般的嘲弄一个个变成敌人感觉就像每件事我因来不及而失去控制这是一段很的旅程直到我找到回家的路是走向你走向你

The sedimentary facies, reservoir petrology, digenesis and the factors influencing on reservoir of Chang 6, in Wu 410 well region are studied.in the end ,the reservoir are sorted and evaluated by sand body distribution, diagenesis reservoir facies,classification of pore texture etc.

应对油田开发的需要,本文在研究时,对各小层进行了详细的对比和研究,依照沉积旋迴,将6_1划分为6_1~1、6_1~2层,每层均具有厚薄不均的3层砂层,其6_1~(1-1)、6_1~(1-2)、6_1~(1-3)和6_1~(2-1)、6_1~(2-2)、6_1~(2-3)等单层砂层,在平面上均可进行对比和研究。

The basal diameter, height of aerial stem, leaf length at middle stem, leaf width at middle stem, internode length at middle stem, internodes number and panicle length of 30 plants from every population were recorded. The statistics of morphological characters showed that the distribution trends of the averages of morphological characters are similar among populations. However, the coefficients of variation within population of 7 morphological characters were very different. The CV of internodes was largest and the CV of height was smallest within population. F-statistics showed that the differences of all morphological characters among populations were significant (P.01). But the differences among populations were different between different groups. The cluster analysis proved that all populations could be divided into three types: salty reed, freshwater reed and giant reed.

对来自每个种群的30个个体的基径、株高、中部叶、中部叶宽、中部节间、节间数、穗7个形态特征的统计分析表明:各形态特征平均值在种群间的分布趋势相似,但变化幅度不同,株高、叶等营养特征变化较大大,生殖特征穗的变化较小;7个形态指标在种群内的平均变异度从大到小依次为中部节间、中部叶宽、穗、中部叶、基径、节间数、株高,种群内的平均形态变异度与生境异质性有关;7个形态指标在种群间均差异显著,但多重比较分析显示显著差异主要存在于BZH、淡水生境种群和盐渍化生境种群之间,在相似生境种群间的形态差异不显著;以形态特征为依据的聚类分析支持将15个种群分为三类:盐生芦苇、淡水芦苇和巨型芦苇。

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质片麻岩、闪质片麻岩、英云闪质到花岗闪质片麻岩和块状二花岗岩组成。岩石地球化学和SmNd同位素特征表明,辉质片麻岩和闪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。英云闪质和花岗闪质岩浆形成于下地壳玄武质岩石部分熔融,而二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。

Scape usually longer than leaves, with 2-3 flowers each with 1bract, floral bract hooded, broad-ovate, as long as ovary, blunt and usually 3-lobed at apex; flower green-yellow, dorsal sepal white with yellow-green veins and green base, elliptic, 4-4.5cm long, short-pointed at apex, keeled on back, pubescent at base inside, petals very long, pendulous, twist, linear, 8.5-12cm long,6mm wide in middle; lip reversed helmet-shaped, longer than dorsal sepal, with claw almost as long as hood, side lobes inflexed, auricles large and nearly broad-triangular; staminode obcordate; stamens with thick and short filaments; ovary rostrate, 5.5cm long, glabrous.

花茎常于叶,具2~3朵花,每花具一枚苞片,花苞片兜状,宽卵形,和子房等,顶端钝而常3浅裂;花绿黄色,重萼片白色而有黄绿色的脉和绿色的基部,椭圆形,4~5.5cm ,短尖,背面具龙骨状突起,基部内侧被短柔毛;花瓣极,悬垂,扭曲,条形,8.2~12cm ,中部宽约6mm ;唇瓣倒盔状较中萼片,具爪,爪几乎和兜等,具内折侧裂片,耳大而近阔三角形;退化雄蕊倒心形,上面基部具一个角状突起;雄蕊具短粗的花丝;子房具喙,约5.5cm ,无毛。

In the K-Na-Ca diagram, intermediate part has the tendency of toellite, and acid part has the tendency of calc-alkaline. According to the above data, its tectonic setting is thought to be continental arc.

其序列组成为石英闪岩-花岗闪岩/斜花岗岩/英云闪岩-二花岗岩组合,二花岗岩略多,地球化学特征具典型造山花岗岩特征,K-Na-Ca图解中性段具英云闪岩趋势,酸性段呈钙碱性趋势,其构造坏境为大陆弧。

During the paleo-geography evolution, inland lacustrine basin began to form, and the two delta skirt in east and west lakeshore are primary formed in Chang 10, lacustrine basin subsidized quickly, lake district enlarged rapidly and destructive delta are developed in Chang 9, delta are more developed in Chang 8, lakeshore line move outward at large range, turbidite developed well near west lakeshore, delta range is decreased in east lakeshore in Chang 7, features of lacustrine basin are changed remarkably, deep lake and half deep lake area is decreased greatly, while delta sedimentary system is developed at its most in Chang 6, framewok is inherited better, but delta′s construction is slowed and is swamping at large scale in Chang 4+5, lacustrine basin began to be silting, shrinking and dying out, and riverway gradually developed well since Chang 3, distributary riverway developed best in Chang 2, because of imbalance subsidence, subsidence center is formed in east Zichang area and in which lacustrine turbidite is sedimented.

在古地理演化过程中,10期内陆湖盆开始形成,东西两岸两大三角洲裙初步形成;9期湖盆快速下沉,湖区迅速扩大,三角洲多为破坏性的;8期三角洲进一步发育;7期湖岸线大幅度向外推移,西部浊积岩发育,东部三角洲面积明显减小;6期湖盆面貌发生了显著的变化,深湖-半深湖面积大大减少,三角洲沉积体系极为发育;4+5期继承了6的沉积格局,三角洲建设进程减慢,三角洲大面积沼泽化;从3期湖盆开始逐步淤浅、萎缩、消亡,河道逐渐发育;2期分流河道发育;1期由于差异沉降,在东部子一带形成沉降中心,沉积了湖相浊积岩。

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