隆起区的英文

• upwelling area

• "隆起"英文翻译    rise; tuberositas; bulge; pr ...
• "区"英文翻译    H region; H
• "隆起区域" 英文翻译 :    upwarped district
• "隆起" 英文翻译 :    [地质学] rise; tuberositas; bulge; protuberate; eminentia; hump; uplift; upheaval; heave; intumescentia; lifting; cripling; swelling; scabrosity; welt; symon fault; hoove-up (指底板); raise; tenting; eminence;◇隆起带 upwarping zone; uplifted zone; 隆起区 bulge region; rise region; 隆起翼 rise flank
• "背隆起" 英文翻译 :    dorsal hump
• "底隆起" 英文翻译 :    bottom heave=basal heave
• "额隆起" 英文翻译 :    frontal eminence
• "腹隆起" 英文翻译 :    ventral tubercle
• "古隆起" 英文翻译 :    palaeohigh
• "后隆起" 英文翻译 :    after wale; after-wale
• "眶隆起" 英文翻译 :    orbital tubercle
• "隆起, 隆凸" 英文翻译 :    eminelntia
• "隆起,隆凸" 英文翻译 :    eminentia
• "隆起；平错" 英文翻译 :    heave
• "隆起；上升" 英文翻译 :    upheaval
• "隆起部" 英文翻译 :    crown
• "隆起处" 英文翻译 :    bumcontact; bumpad
• "隆起带" 英文翻译 :    mole track
• "隆起的" 英文翻译 :    bulbous; embossed; intumescent; protuberant; ridgy
• "隆起谷" 英文翻译 :    valley of elevation
• "隆起脊" 英文翻译 :    rise crest
• "隆起块" 英文翻译 :    bump
• "隆起山" 英文翻译 :    domed mountain
• "隆起物" 英文翻译 :    bunch; hunch; protrusion; protuberance; ridge
• "隆起线" 英文翻译 :    ridge

• So it can be concluded that there did not exsit regional compressional folded - uplifted area which was eroded widely in mesozoic in the west neighouring district
  这表明中生代在盆地西邻不存在广泛遭受剥蚀的区域挤压褶皱隆起区。
• However , the large - scale erosions in the uplift areas of the fault belt and the surrounding margins allow the determination of the fault active periods to be difficult
  在断裂带和外缘的隆起区地层剥蚀程度较大，活动时间的厘定比较困难。
• The migration of hydrocarbon tends to take place from high pressure stress distribution area ( hydrocarbon generation sag ) towards low pressure stress distribution area ( uplift )
  油气从高压应力分布区(生烃凹陷)向低压应力分布区(隆起区)运移。
• Results the result on this sedimentary environment was an offshore terrigenous fresh water lake from permian of shiqanfeng formation marinecontinental transitional facies in the southern of north china
  结果研究区地层自南西向北东呈现依次增厚的趋势，整体为北东方向倾斜的宽缓斜坡环境；砂岩分布特征指示物源来自南部隆起区和沉积中心在研究区以北地区。
• The special aerial magnetism , gravity and mt at chasang segment in the western uplifting district show that it is superposed by two or three large - scale south dipping structural block with east - west strike . the closure of bangong lake - dingqing limited ocean and the further gathering of neighboring blocks later form it
  西部隆起区查桑段特殊的航磁、重力和mt显示其由2 - 3个近东西向大型南倾构造块体叠覆而成，受班公湖-丁青有限洋关闭和相邻地块进一步汇聚形成。
• ( 1 ) abnormal high velocities mainly exist around qingzang plateau , especially in junggar , tarim , qaidam and sichuan basin , velocities there are higher than 8 . 2 km / s . ( 2 ) low velocities only exist in the middle of qingzang plateau and western part of sichuan and yunnan region . in eastern china , low velocities are predominant
  整体上中国东西部存在明显差异，西部地区速度变化以高速异常为主：高速异常区主要是沿青藏高原隆起区的周边分布，特别是准噶尔盆地、塔里木盆地、柴达木盆地及四川盆地都呈明显的高速，均超过8 . 2km / s ；青藏高原隆起区的中部，显示出速度的低异常带；位于青藏高原东南缘的川滇西部地区速度呈现低异常。
• 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。
• The regional deformation anomaly of medium - term phase ( 1 ~ 3 years or more ) before strong earthquake occurrence usually shows three aspects of common characteristics : for regional vertical deformation , it shows distribution features of anomalous uplift area and concentration belt - high gradient belt of vertical differential deformation ( some of them reflect distribution of four quadrants ) related to tectonics ; for horizontal movement , it shows features of centralized high strain area ( or zone ) of domination shear deformation related to active blocks and faults ; it shows common features of regional vertical deformation anomaly area and high strain distribution area of horizontal deformation
  摘要强震前中期阶段（ 1 ~ 3年或稍长）区域性形变异常往往表现出3个方面的共性特徵：区域垂直运动变形呈现与构造有关的异常隆起区、垂直差异变形高梯度带（有的还呈“四象限” ）分布特徵；水准运动变形呈现与活动地块及断裂构造有关的、以剪切变形?主的高应变集中区（带）特徵；区域性垂直形变异常区与水准形变的高应变分布区共性的特徵。
• The authors hold that the joint actions of numerous factors such as the upper mantle uplifted zone ( the mantle thinned zone of lithosphere ) , the upper mantle anomalous area ( relatively low - velocity area ) , the uplifted zone of intracrustal high - conductivity layer , the deep fault ( shear zone of lithosphere ) , the margin of the crust - upper mantle uneven masses , the basement uplifted area reflected by gravity high , the magmatic belt and tectonic intersection reflected by skipped magnetic field , control the distribution of auriferous skarn deposits and copper ( associated with gold ) skarn deposits
  作者认为，上地幔隆起带（岩石圈地幔减薄带） 、上地幔异常区（相对低速区） 、壳内高导层隆起带、深断裂（岩石圈剪切带） 、地壳上地幔不均匀性块体的边缘、重力高反映的基底隆起区、跳跃磁场反映的岩浆岩带和构造交汇处等诸多因素的共同作用控制著含金夕卡岩矿床和铜伴生金夕卡岩矿床的分布。