浅灰的

Hybrids of carbonate and terrigenous sediments Carbonate with terrigenous sediments are of characteristic from Emsian to Eifelian in stable shallow-sea faciesregion in Longmenshan area, and they can be classified evidently into hybrid Ⅰ and hybrid Ⅱ(Jingbaoshi-type). Type Ⅰ produced in mud shelf setting occupied hundreds of tempestite beds in which bottom cast、 hummocky cross bedding sandstones、 coquina were inter-beddded with shales that beared a great deal of verm traces、 bioturbations、 benthic communities dominative of brachiopods. Type Ⅱ in sand-mud-marl shelf was characterized by high-energy foreshore sandbeach facies and shelly bank facies.

碳酸盐与陆源碎屑混合沉积方面对微相、相特征、旋回样式、沉积机理研究表明，龙门山地区泥盆纪稳定浅海相区Emsian期和Eifelian期混合沉积十分发育，颇具特色，明显可以划分为两种类型：混积Ⅰ型，泥质陆棚背景下发育风暴沉积组构，幕式风暴期产生具丘状层理、底流冲刷构造的钙质砂岩、介壳岩，平息期则形成具大量虫管和生物扰动的深灰色、黄绿色页岩及海百合茎灰岩，腕足动物等大量繁盛；混积Ⅱ型，砂泥灰质陆棚背景下以发育高能前滨沙滩及生物介屑滩为特色，近滨至陆棚的砂泥灰互为混合，三者比例接近，肉眼难以区别确切岩石类型。

She rushed into her room straightaway, of course, but I saw her stained white housedress and the mass of dirty, pigeon-gray feathers on her head.

她直接冲进自己的房间，当然，我只看到她脏兮兮的白睡衣和满头乱糟糟的浅灰羽毛。

As the lake basin shoals and silts up, the color of clastic sediment gradually changes from black, black gray, gray and grayish green to purplish grey and red purple, meaning that the subaerial alluvial fan deposit of late stage has replaced the fan-delta deposit and that the coal-forming process ends.

待湖盆逐渐变浅和淤积，碎屑沉积物的颜色由黑、黑灰、灰、灰绿逐渐变为紫灰和紫红，表明晚期陆上冲积扇沉积已经代替了扇三角洲沉积，成煤作用随之结束。

A soft, pure, earthy, fine-textured, usually white to light gray or buff limestone of marine origin, consisting almost wholly (90-99%) of calcite, formed mainly by shallowwater accumulation of calcareous tests of floating microorganisms and of comminuted remains of calcareous algae (such as cocoliths and rhabdoliths), set in a structureless matrix of very finely crystalline calcite.

中文解释=海产起源的石灰石，柔软、纯净、土质、组织精细，通常从白色到浅灰或浅黄色，几乎完全（90-99％）由方解石组成，主要由浮游微生物的粉碎残留物浅水堆积而成，嵌在非常精细的方解石晶体的无定形填质中。

Factory long-term production, export granite basin boards have Units: English brown, dark green linen, brown diamond, red diamond, gold diamond, purple Golden Ma, India blue, butterfly green, Sicily, jute, etc.; marble has: Spain Beige Indonesia beige, beige Myanmar, Oriental white, shallow Jinfeng, white Begonia, red bars hang the gray matter and white bars hang ash,, black root, blue red cream, coffee and so on.

本厂长期生产、出口的花岗石面盆台板有：英国棕、墨绿麻、啡钻、红钻、黄金钻、紫点金麻、印度兰、蝴蝶绿、西西里黄麻等；大理石有：西班牙米黄、印尼米黄、缅甸米黄、东方白、浅金丰、白海棠、红筋杭灰、白筋杭灰、金香玉、黑白根、青红奶油、咖啡等。

The water splashed quietly along a course of round, dove-colored stones, eddying noisily around the twisted branches that had tumbled into the stream, disappearing at last into a thicket a few yards below.

溪流一路流淌，静静地冲涮着沿路的圆形的、浅灰略带紫红色的石头上，而在那些掉落到溪水中的弯曲的树枝旁，这溪水便发出声响，形成旋涡，最终，这溪水流入了下游，几码远之外，那些灌木丛中，失去了影踪。

Reefs, reef-mounds and lime mud mounds are all carbonate buildups, and the reefs and banks are important targets for petroleum exploration The reefs, banks and mounds should be divided from each other not only in theory, but also in exploration practice, because of so many differences in sedimentary compositions, fabrics, environments, distribution in time and space, and the characteristics of petroleum geology If the original reef or bank itself was fine reservoir rocks, then it would become a better reservoir after the reservoirconstructive diagenesis The formation of a high quality carbonate reservoir is controlled by two factors: the sedimentary microfacies and the reservoirconstructive diagenesis The first is the basis for the formation of a high quality reservoir, and with the high energy reefbank facies as the best; the latter includes the cataclasis, the dolomitization and the karstification The dolomitization and karstification are the best for the formation of a high quality reservoir The karstification has the widest distribution, profoundest effect, and plays a vital role in the high quality reservoir forming The karst types are quite rich in the limestone reef or bank reservoir, including synsedimentary karst, penesedimentary karst, supergene karst and hydrothermal karst, and so does the dolomitization reef or bank reservoir The formation mechanism of synsedimentary karst and penesedimentary karst is related to the short time exposing and leaching of the cyclical highfrequency shallowupward sequence when the reefs or banks are forming The supergene karst is controlled by the exposing and leaching of tertiary cyclic sequence type I interface after the reefs or banks forming Thus, there developed a great deal of secondary corrosion pores, corrosion fractures and huge caves besides some original pores remained in the reef and bank reservoir Scarcely there are any original effective pores in reefmounds and lime mud mounds, especially in senkes among mounds, but secondary pores could be formed by karstification, and there would likely develop source rocks with high organic abundance

礁、礁丘、丘同属碳酸盐建隆，礁、滩是重要勘探目的层。但各自在沉积组分、组构、环境和时空分布，以及油气地质条件上迥然不同，因而无论从理论还是勘探实践上，都有必要将其各成体系划分开来。礁滩自身为好储集岩，当建设性成岩作用叠加后可形成好的储层。碳酸盐岩优质储层形成，主要受沉积微相与建设性成岩作用两大因素控制。前者是基础，并以高能的礁滩相带为最好；后者主要包括破裂、白云石化和溶蚀三大类，并以白云石化或溶蚀为最优，其中的溶蚀分布最广泛、影响最深刻而对优质储层形成起决定性作用。礁滩储层中的古岩溶类型最为丰富多彩，包括同生期、准同生期、表生期和埋藏期热流体岩溶的所有类型，白云岩化礁滩体也不例外。其中，同生准同生期岩溶的形成机制与礁滩沉积时高频层序旋回向上变浅序列的短暂暴露淋溶有关，表生期岩溶则受控于礁滩沉积后三级层序旋回Ⅰ型界面的暴露淋溶。由此，导致礁滩储层中除了可以也是唯一保存原生孔隙外，还发育了次生溶蚀孔洞缝和大型溶洞。礁丘、灰泥丘尤其是丘间洼地中发育高有机质丰度烃源岩；它们自身没有有效的原生孔隙，但岩溶作用可以形成次生孔隙。

Grew out of the VALAFRANCA are still full of LONDONFOG classic and romantic charm, but the oil blue, light gray and other fashion colors, self-cultivation version of the coat, filled with nostalgic sense of fashion uniforms, but also felt the winds of fashion VALAFRANCA have completely gone beyond LONDONFOG, such as the flood hit to my eyes.

脱胎于LONDONFOG的VALAFRANCA依然充满了经典与浪漫的韵味，但石油蓝、浅灰等时尚的色彩，修身版的风衣，充满怀旧感的时装化军服，又感觉到VALAFRANCA的时尚之风已经完全超越了LONDONFOG，如潮水般向我的眼睛袭来。

Dun -(1) first stage in the adult mayfly's life cycle; usually of short duration (1 to 24 hours); this is the stage most often imitated by the dry fly;(2) a darkish gray-blue color that is very desirable in some fly tying materials.

1蜉蝣的第一生命阶段，很短，一般1-24小时（2）浅灰兰色的用于绑制毛钩的材料。

B light to intermediate transfer website performance is if the full-color printed a thick and strong, can be used instead of ultrafine 300, 400-mesh point to no buyang, but there are in the supporting this super fine wire is not a good business card printing and membership card production, resulting in the whole-tone, so use with four color separation business card printing and membership card production, decreased slightly in the optical Department, dot by LC, LM on magenta and supplemental lighting of a thick and are some of the use of laodelphax LB the light grey, LR on peach, LG 浅紫 light-green, LV, and so on secondary light-coloured, and this is the kind of color by the car and it came to technical method of extension, how to make sure the complementary color concentration and minus four dot color separation, is out on the relationship between the original and buyang is the most difficult technical staff must villagers'participation.

平部到洋间调的网不面表示不若印满版色菲薄无力，可以改用超粗300线、400线以上钩不面来弭补，但有见於这栽超粗网线并欠好制卡和会员卡制作，造不败整版色调不佳，所以改用以四色版制卡和会员卡制作，在平部稍降网不面百分比，由LC不深蓝、LM不深洋赤等来补平部之菲薄感有些搁置LB灰不深灰、LR不深桃、LG不深红、LV不深紫等二不主色不深色为之，这是栽由手工开色石版法蔓延来的技艺，如何拿捏补色浓度及增去原有四色版网不面百分比，是开不入来本来及补不出色版时技艺职员最不易也是务必的考量。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。