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Home > chinese-english > "盆地区" in English

English translation for "盆地区"

cuvette reg. de la
cuvette, reg. de la


Related Translations:
干盆地:  waddywadiwady
盆地沼泽:  basin mire
吐鲁番盆地:  turfan depression
次盆地:  subbasin
蓄水盆地:  reservoir basin
孤立盆地:  isolated basin
大陆架盆地:  continental shelf basin
地质盆地:  geologic basin
大地盆地:  geobasin
伦敦盆地:  london basin
Example Sentences:
1.Breakthrough in mineral exploration using geogas survey in the basin area of northern qilian region and its significance
地气测量在北祁连盆地区找矿突破及其意义
2.By using the standard deviation method , the scaling properties described by the local fractal dimension d and crossover length tc of 48 measured landform profiles in different direction of 6 different studied landform sections are calculated
负反馈机制表现的越明显;对于以构造沉降作用为主的盆地区而言,各个方向的地形剖线的分维值均显示出小于1 . 5的正反馈机制。
3.In this area , there are obviously different crustal tectonics within the basins and mountains displaying that the thickness of crust in the mountain areas is greater with obvious " mountain root " and thinner in basin areas
已有资料表明,在中国西北盆山地区,山脉和盆地具有明显不同的地壳结构,它们的地壳厚度不同,表现为山区地壳厚,具有明显的山根;盆地区地壳厚度小。
4.In conclusion , it tables a proposal that it divided the sichuan into three sections : the basin section , the mountainous area in the southwest sichuan , the altiplanos section in the western sichuan then it recommends the pavement structure applied to different nature climate condition and different grade highway
本文针对四川省高等级公路路面结构的使用情况,并对以后的发展作了展望,提出了把四川省划分为盆地区、川西南山区、川西高原区三个分区,推荐了适用于不同自然气候条件和不同等级公路的路面结构。
5.( 2 ) in southern china , the velocities are near average value . a little low velocities exist in the regions such as zhujiangkou , middle of guangxi , lushan and so on . a little high velocities exist in the middle region lied to the south of yangzi river and to the north of zhujiang river
东部地区速度变化以低速异常为主:整个华北和东北地区,都呈现pn低速异常,特别是华北盆地区、渤海湾和山西地堑低速异常非常明显,最小低于7 . 8km / s ;华南地区整体上在平均值上下,在珠江口地区、广西中部地区、庐山地区波速略微偏低,在长江以南,珠江以北地区中部波速略微偏高。
6.The fractal dimensions of elevation isolines in 6 studying sections from 3 different types of geomorphological zones , including high mountain , low - moderate mountain and catchment basin , are computed by using successive coarsening method . the results show that all the studied isolines are statistical fractals , and the fractal dimensions take on different characters for different geomorphological types and scale ranges
在0 . 1 - 10km标度范围内,等高线分维值总体表现为最新隆起区(中低山区) >强烈隆起区(高山区)沉积凹陷区(盆地区) ;在5 - 200km标度范围内则表现出强烈隆起区最新隆起区沉积凹陷区。
7.After that , the multifractal spectra dq - q are computed by fixed - mass method . the results show that in the studied scaling range different types of landscapes and profiles in different directions perform different fractal properties , that is , the d value and crossover length ^ decrease in turns with the landform type from high - moutain , mid - low mountain to basin , and the profile parallel to wear grooves often has lower d values ( < 1 . 5 ) than those perpendicular to wear grooves do ( 1 . 5 ) in the same section
提出以地貌分形特点和渡越长度为依据的地貌层次界定方案,研究指出了5km左右应为宏观临界点:不同构造地貌区、不同取向的剖线的多重分形谱值域范围宽窄表现出中低山区高山区盆地区,垂直构造地貌斜坡方向斜交方向平行方向的特点,表明了内外营力作用的不均匀性和方向性。
8.Furthermore , the dq value ranges of profile multifarctal spectra in different landform types and in different directions of the same sections perform different properties and anisotrpies . it can be concluded that the landscape fractal properties depends closely on the int ensity , manner and inhomogenity of exogenic and inogenic processess , and with the properties , we can study quantatively the dynamic geomorphic process . by using the same methods just above , local fractal dimensions d , crossover length tc and the multifractal spectra dq - q of two large - scale landform profiles ( across and along tianshan mountain ranges respectively ) are calculated . the results show that in the studied scaling range the two profiles perform different scaling properties , and both of them can be divided to three evident different linear scaling subsections
不同类型地貌区二维地貌表面也表现出多度域分形特征,而且随着观测尺度的增加,每个区间的分维值均表现为依次减小,表明外营力作用的影响逐渐被内营力作用所取代:不同类型地貌区在相应区间的分维值表现为高山区中低山区盆地区,体现了不同类型地貌表面粗糙性或复杂性的差异,因此分维值大小可作为地貌表面外营力侵蚀作用强度的重要指标:利用标度区的间断点和各种地貌类型表面分维值或宏观效应趋于一致,提出5 - 6km左右可作为地貌的宏观临界点,并且与利用地貌剖线研究所得到的5km这一数值是基本吻合的。
9.In addition , the dq - q curves behave in different shapes . it can be concluded that the scaling properties depend colsely on the way , intensity . acting scale and distribution in space of inogenic and exogenic processes . according to the scaling natures of the two landform profiles , it is proposed that the 5km scale is the low limit of the inogenic process effects which begin to dominate landscape patterns in landform systems
该结果对理论地貌研究具有重要意义:不同地貌类型表面的多重分形谱值域表现为高山区中低山区盆地区的总体特征,地貌表面多重分形谱特征表明了内外营力地貌作用类型和强度在空间上分布的不均匀程度。
Similar Words:
"盆地内自源自生沉积" English translation, "盆地泥炭" English translation, "盆地平原" English translation, "盆地评价" English translation, "盆地前" English translation, "盆地群代" English translation, "盆地融坑" English translation, "盆地山岭" English translation, "盆地山岭相间景观" English translation, "盆地山脉" English translation