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与 成山 相关的网络例句 [注:此内容来源于网络,仅供参考]

Instead, I stand here looking at a mountain that has been torn asunder by some extraordinary force.

但是,当我到达这座山时,这座山似乎被一种未知的巨大力量撕成了碎片。

Since then I have lived to see state after state extirpate its wolves. I have watched the face of many a newly wolfless mountain, and seen the south-facing slopes wrinkle with a maze of new deer trails. I have seen every edible bush and seedling browsed, first to anaemic desuetude, and then to death. I have seen every edible tree defoliated to the height of a saddlehorn.

从那时起,我看着一个又一个州灭绝了狼,我看着一座又一座山成了新的无狼山,我看着纷乱的鹿蹄印儿给朝阳的山坡新添了片片褶皱,我看着一株株灌木和树苗被啃得枯萎,啃到死去,我看着一棵棵可以吃的树,从地面到马鞍那么高之间的叶子全被吃光。

Can become frankpledge as 100, the hamlet becomes old village, a hill by " eat " became bareheaded hill.

可随着一户变成十户百户,小村变成大村,一座座山被"吃"成了光头山。

The " cloud " in the " between pink clouds of white emperor of decline of day of the " in the poem is vapor is encountered cold the Xiaoshui that form drips to gather and be become in float of empty horizontally pivoted hung, the hill of river of liquefacient;" a thousand li in belonging to states of matter to change returns the " in " one day one day to return ", the rate that shows a boat is very rapid,"What " of a thousand li points to is distance,"What a day of " points to is caw of simian sound of time;" two sides does not live ", simian ululation is by simian vocal cords vibration generation, canoe of the;" in relying on air to upload person ear from the bank already crossed " of 10 thousand heavy hill, be it is with hill consult content, the boat is moving,"Canoe " explained the quality of the boat is lesser, and still got water is opposite it up buoyancy.

诗中"朝辞白帝彩云间"中的"云"是水蒸气遇冷形成的小水滴在空中悬浮聚集而成的,属于物态变化中的液化;"千里江陵一日还"中的"一日还",说明船的速度很快,"千里"指的是路程,"一日"指的是时间;"两岸猿声啼不住",猿啼声是由猿的声带振动而产生的,并靠空气从岸边上传到人耳中;"轻舟已过万重山",是以山为参照物,船在运动,"轻舟"说明了船的质量较小,并且还受到了水对它向上的浮力。

These gold deposits are typical orogenic gold deposits, with similar geological and geochemical characteristics that associated with the orogenesis spatial-temporally.

这些金矿床在时空分布和成因上都具有一定的规律和密切的成生联系,具有相似的地质和地球化学特征,金成矿与造山过程有着密切的联系,属于较为典型的造山型金矿床。

Specially made with selected spring tea leaf harvested from aged wild arbor tea trees in Nannuo mountain in Xixuan Pana which yields a light tawny tea liquor with an unique long lasting honey aroma when consumed.

产品说明:选用西双版纳勐海南糯山百年以上树龄乔木茶树早春原料精制而成,汤色透亮,带有南糯山特有蜜香,回味悠长,为龙园号06精品之一。

But recent survey reported that Panicum maximum, a perennial grass in the family of Poaceae and listed as one of the twenty most noxious invasive plants in Taiwan has replaced the role of M sinensis in those areas. As a result of recurrent burning, A. confuse forest has been gradually replaced by the grassland of P. maximum. In this study, I compared morphological, photosynthetic, growth and life history characters of field growing P.

早期的研究指出:在大肚山与铁砧山区的本地植物芒草为当地相思树林反覆火烧后的最优势种;但近年来同一地区的研究显示:大黍已取代芒草的角色,而且发现大黍在火烧后植群覆盖度显著的增加,但芒草却没有相同的现象;反覆火烧使得大肚山地区的相思树林逐渐转变成以大黍为主的草生地。

Combined with the regional data the research indicates that (1) the Tianmenshan main body formed in the Middle Jurassic Epoch, whereas the minor body was the further differentiated and evolutive product of the main body;(2) in the Chongyi-Dayu-Shangyou ore concentrated area, the west of Gannan area, the diagenetic age and metallogenic age are basically concordant, and the mineralization concentrated during 150~155 Ma;(3) from the middle-plutonic granite intrusion to the hypabyssal granite-porphyry vein, the magmatic activities experienced only 1~5Ma, indicating there was the concentrated period of mineralization.

结合区域资料,研究表明:①天门山岩体的主体形成于中侏罗世,补体是主体进一步分异演化的产物;②在赣南西部的崇余犹矿集区内成岩与成矿的年龄基本上是协调一致的,成矿集中期为150~155 Ma;③岩浆活动由中深成相花岗岩侵入体演化到浅成相花岗斑岩脉仅相差1~5Ma,表明存在成矿集中期。

These results suggest that the diagenesis material of the Xiangshan volcanic intrusive complex was derived from crustal sources. The sources either had relatively lower maturity or had more juvenile mantle-derived igneous rocks than the exposed basement metamorphic rocks. Involvement of a small amount mantle-derived magma during the formation of the Xiangshan volcanic-intrusive complex was also possible. The diorite enclave, sub-quartzmonzonitic porphyry and lamprophyre were probably different mixing products between mantle and crust materals.

上述同位素示踪结果充分证实:相山火山-侵入杂岩的成岩物质主要为壳源,但与该区出露的基底变质岩相比,其物源区的成熟度相对较低或含有一定量的火成物质,并且不排除在其成岩过程中少量地幔物质的介入;闪长质包体、次石英二长斑岩及煌斑岩的成岩物质均含有一定量的地幔组分,可能为壳-幔混合作用的产物,只是受地壳物质混染的程度不同而已。

The reservoir rock types in the region of interest are grain limestone, algal limestone, cryptite, siltstone, muddy limestone and mudstone. The thesis identified as a result of changes in the deposition causing the heterogeneity in plane, and then the geological oil reserves have been calculated in accordance with the areal heterogeneity.3、Based on the data of core analysis, bore logging, array induction imaging log and FMI, porosity and permeability model were built using regression analysis. Through testing 45 rock samples, a, b, m, n value were obtained and used to calculate single-layer oil saturation value using the Archie formula. According to the theory of laterolog and inductolog, resistivity ratio and cross plot were used to identification effective thickness. Effective thickness was identified delicately in 103 wells. Based on the over work, active porosity and oil saturation was calculated accurately.4、According to observation of 100 pieces of the thin slices, cast thin slices and 383m core in three wells, the chief diagenesis in this area were compaction, cementation, denudation and cataclasis. Cementation and denudation were universally influenced active porosity this area. The intergranular pores, residual pores and secondary pores were formed in thin carbonated reservoir of lacustrine facies.5、The influence of reservoir heterogeneity to reservoir calculation was analyzed systematically using actual data. And the conclusions were as follows:①The principal reason leading to oil distribution unequal is interior structural feature of reservoir in structural hydrocarbon reservoir.

确定了由于沉积微相的变化而导致的平面非均质性,进而在平面上按照平面非均质单元计算了石油地质储量。3、利用岩心分析、常规测井曲线与阵列感应、成像测井资料相结合,分岩性利用回归分析方法建立了储层孔隙度、渗透率模型;通过对45块岩样进行岩电试验,获取了a、b、m、n值,利用阿尔奇公式计算了各单层含油饱和度值;根据侧向电阻率和感应电阻率串并联特性,利用电阻率比值法与常规交会图法相结合重建了有效厚度图版,对全区103口井目的层段进行了有效厚度精细划分,通过以上工作,准确求取了储量计算单元内有效厚度参数、有效孔隙度参数以及含油饱和度参数。4、通过对研究区3口井383m岩心观察,100余块薄片、铸体薄片镜下鉴定得出:油泉子油田上、下油砂山组储层主要成岩作用是压实作用、胶结作用、溶蚀作用和破裂作用,其中溶蚀作用、胶结作用最普遍,这两种作用对有效孔隙度影响最大,以上成岩作用形成了原生粒间孔、粒间残余孔和次生孔隙(如粒间溶孔、粒内溶孔、铸模孔、晶间孔等)为主的薄层湖相碳酸盐岩储层。5、利用实际资料,系统分析了油藏非均质对储量计算的影响,认为:①对于构造油气藏而言,油气藏构造及断裂特征是造成油气分布不均的首要原因,储集条件相同的条件下,构造高部位有利于储存油气,油气在垂向的重力分异体现了油气藏内部构造的不均一特征。

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