第四系 的英文怎麼說

中文拼音 []
第四系 英文
quaternarysystem
  • : Ⅰ助詞(用在整數的數詞前 表示次序) auxiliary word for ordinal numbers Ⅱ名詞1 [書面語] (科第) gr...
  • : Ⅰ數詞(三加一后所得) four Ⅱ名詞1 [音樂] (中國民族音樂音階上的一級) a note of the scale in gong...
  • : 系動詞(打結; 扣) tie; fasten; do up; button up
  • 第四 : fourth第四產業 quaternary economic sector
  1. The fault faults from basemet to quaternary system, and has the feature of contemporaneous and normal fault

    該斷裂自基底一直斷到第四系,具同生正斷特徵。
  2. The intense eluviation and weathering of soil with groundwater and run - off result in the enhancing of capacity of transference of some elements, such as si, al, fe, mn. the chemical reactions of the colloid particles in the soil water make those crannies or holes filled by some epigenetic clay minerals and quartz. then a great deal of white reticulate clay comes into being in the quaternary laterite of the dongting basin

    地下水和地表水強烈的淋溶作用使土壤中硅鋁鐵錳等元素的遷移能力增強,土壤膠體粒子之間的化學反應,使得這些孔隙空間在後期逐漸被次生黏土礦物和石英所充填,最終,在洞庭盆地第四系紅土地層中形成大量的蠕蟲狀和根狀白色網紋。
  3. The quaternary system is characterized by high geothermal gradient, with low scope of overpressure in its deep and shale caprock saturated with formation water of high salinity

    第四系具有較高的地溫梯度,深部發育了低幅超壓;甘森泉小柴旦基底斷裂影響氣藏構造的完整性;第四系飽含高礦化度地層水泥巖構成的蓋層可以起到一定的封蓋作用。
  4. The basin has dual texture in which it is horst - graben in mesozoic - eogene and " plate " depression in tertiary - quaternary. the basin is the complex basin with wresting and extending dynamic properties, called as torsion - extension basin

    「盆地」具有雙層結構的特徵,下部的中生界及下為壘?塹結構,上部的第四系為「碟」狀的坳陷結構。
  5. There are many salt dome structures within the salt sediment group

    鹽上層?上二疊統一第四系
  6. The authors studied the characteristics of element geochemistry, mineral assemblage and microtexture of the white reticulate clay in the quaternary laterite of the dongting basin with some experimental analysis methods, such as chemical analysis, x - ray diffraction analysis, ir and sem analysis. the genesis of the vermiculate reticulate clay and the rhizomatic reticulate clay in the quaternary laterite of the dongting basin are discussed. the formation of crannies or holes in the soil and the transference of soil elements are absolutely necessary conditions to form the white reticulate clay in laterite

    在野外考察的基礎上,運用化學全量分析x射線衍射分析紅外光譜分析和掃描電鏡微形貌分析等實驗方法和手段,對洞庭盆地第四系紅土地層中網紋的元素地球化學礦物組合特徵和微形貌特徵進行了統研究,對洞庭盆地紅土地層中2種主要的網紋類型蠕蟲狀網紋和根狀網紋的成因進行了探討。
  7. Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western, and moves towards south and deeper along carbonate rocks, then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ), and then mainly transforms into the horizontal drainage in the loess layer of quaternary, finally drains in lu - botan depres sion

    並且提出,關于對統南界的認識,是否存在另一可能:即在西部碳酸鹽巖裸露區大氣降水入滲后,沿碳酸鹽巖向南向深部運動,然後,並非在極小的水力坡度驅動下長距離地向東部黃河、泉群徑流排泄,而是通過上覆厚度約400m的向上運動,繼而主要在第四系黃土層中轉為向南水平排泄到鹵泊灘。
  8. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據三塘湖盆地殘餘地層序列、沉積體、沉積充填特徵和原型盆地恢復,以及不同構造層的構造變形特徵的綜合研究分析,認為三塘湖盆地經歷了如下個發展演化階段:前二疊紀盆地基底發展演化階段;二疊紀斷陷-拗陷盆地發展演化階段; :三疊-侏羅-白堊紀拗陷盆地發展演化階段;三-第四系新生代盆地發展演化階段。
  9. Prediction of quaternary aquifer water inflow in mine shaft of liliangdian

    李糧店第四系井筒涌水量預測
  10. Based on the geological and mining conditions and occurrence characteristics of loose aquifer of xinglongzhuang colliery, water bursting cause of 4303 full - mechanized caving mining face under loose aquifer was analyzed, the prevention measures of the 3rd aquifer and reasonable dimension of coal pillar for sand proof were discussed in this paper

    摘要根據興隆莊煤礦地質采礦條件,結合鬆散含水層賦存特徵,分析了采區4303綜放工作面第四系鬆散含水層出水的原因,探討了防治三含水的技術途徑和留設防砂煤柱的合理尺寸。
  11. The forcast and assessment on earthquake stonebrash liquefaction of the yellow river delta had been analysed and worked over synthetically and closely for the first time in the history, eventually, it was proved that the earthquake stonebrash liquefaction was the predominant disaster in the yellow river delta and several regions would bring about earthquake stonebrash liquefaction disaster when the intensity of an earthquake was 6 degree

    開展了黃河三角洲第四系沉積特徵方面的研究4首次全面的對黃河三角洲地區地震砂土液化進行區劃和預測評價,提出地震砂土液化是黃河三角洲主要的地震地質災害,當地震烈度為時,部分地區將產生液化的新觀點。
  12. Based on the analysis of the late cenozoic stratigraphy, neotectonic topography and the structures of quaternary in the region, the present paper studies the neotectonic characteristics of the region systematically

    通過對晚新生代地層、新構造地貌及第四系內褶皺和斷層的綜合分析,闡述了區內新構造活動特徵。
  13. Thin interbedded sands and shale, and loose reservoir are main sedimentary character of the quaternary system of target formation in this area

    本區目的層第四系以砂泥巖薄互層、儲層巖性疏鬆為主要沉積特徵。
  14. Based on its special geological and mining conditions of qidong colliery, the cause of water bursting of loose aquifer in the 4th lineage in 7 ( subscript 1 ) 14 full - mechanized mining face of the first mining area was analyzed and technology method of preventing the 4th loose aquifer was discussed according to the occurrence characteristics of loose aquifer and damage characteristics of overburden rock in 7 ( subscript 1 ) coal seam

    摘要根據祁東煤礦特殊的地質采礦條件,結合鬆散含水層賦存特徵及7 (下標1 )煤層覆巖破壞特點,分析了一采區7 (下標1 ) 14綜采工作面第四系鬆散含水層出水的原因,探討了防治含水的技術途徑。
  15. This text has introduced the research background, the research purpose and research current situation of the small cities and towns question at first, secondly analyzed the intension of small cities and towns development and theoretical foundation, and through the small cities and towns develop analysis of function to the present stage, propose small cities and towns help and raise peasant income, help and promote surplus rural labor force shift, favorable to the developments of township enterprise etc. by development ; the third, develop analysis of the current situation according to the small cities and towns of hebei province, point out the question existing in the development of small cities and towns of hebei province, and the development level to the small cities and towns of hebei province has been evaluated, think that the development of small cities and towns of hebei province is in stage of starting ; the fourth, the restriction factor in infrastructure investment, function reforming, financial management system and construction plan of government etc. existing in the construction of the small cities and towns of hebei province of network analysis ; at last, it propose hebei province small cities and towns the areas of developments strategic and government function not bring about an advance in small cities and towns of hebei province, household register, people, industrial structure adjustment and relevant countermeasures, such as overall arrangement, land utilizing, fund, planning and environmental protection of the industry etc

    但是河北省小城鎮發展的步伐明顯落後于全國平均水平,更落後于沿海發達省份。本文首先介紹了小城鎮問題的研究背景、研究目的以及研究現狀,其次分析了小城鎮發展的內涵和理論依據,並通過對現階段小城鎮發展作用的剖析,提出小城鎮發展有利於提高農民收入、有利於促進農村剩餘勞動力轉移、有利於鄉鎮企業的發展等;三,根據河北省小城鎮發展現狀的分析,指出河北省小城鎮發展中存在的問題,並對河北省小城鎮的發展水平進行了評定,認為河北省小城鎮發展處于起步階段;統分析了河北省小城鎮建設中存在的基礎設施投資、政府職能改革、財政管理體制以及建設規劃等方面的制約因素;最後,提出河北省小城鎮發展的區域戰略以及促進河北省小城鎮發展的政府職能、戶籍和人口、產業結構調整和產業布局、土地利用、資金、規劃和環境保護等相關對策。
  16. These strata of basin are made up of cretaceous period, tertiary period and quaternary period. tertiary period is the major sediment in the basin and the biggest thickness is up to five thousand meters. this thesis studies the petrology and characteristic of the diagenetic process of the reservoir

    盆地的沉積巖主要由白堊、上下第四系組成,下是盆地中的主體沉積,最大厚度5000米,分為萬昌組、永吉組、奢嶺組、雙陽組。
  17. It is possible for the terminal activity faults to penetrate to the quaternary, but their scale is generally small and the penetrating distance is short, therefore, they can not induce earthquakes on a large scale. the remote sense images of last thirty years in daqing region show that the linear tectonics have not changed remarkbly, in the meantime, the earthquake timing figure shows that the probability of the faults inducing earthquakes, which ms is no less than 5, is little, though some terminal active faults have penetrated to the quaternary

    晚期活動斷裂有可能斷至第四系,但規模小,延伸的距離短,不會引發大規模地震,遙感解譯分析表明, 30多年來衛星遙感影像顯示的大型線性構造並無明顯變化;另外結合大慶地區地震時序圖認為,晚期活動斷裂即使斷至第四系,其活動引發5級以上地震的可能性也極小。
  18. The basin has three evolutionary stages including intracontinental rift basin in p1 - p2, down basin in t2 + 3 - k and the strong trust - orogeny process in n - q. according to the unconformity contact relationship and sedimentary components, santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement, pi - p3 tectonic sequence, t - k tectonic sequence and n - q tectonic sequence

    根據盆地地層之間的不整合接觸關,考慮到各層序沉積物組成與生物組合特徵等因素,將三塘湖盆地劃分為: ( o ? c )基底構造層序,二疊( p )構造層序,三疊( t ) ?白堊( k )構造層序和第四系構造層序。
  19. In view of the reality of the thick quaternary system and low strength of the luocun - xiaonengchang dump foundation and in combination of the dumping technology adopted, the analysis of the foundation carrying capacity and slope stability are made so as to determine the structural parameters and to provide data for the dump operation

    針對姑山礦羅村小農場排土場地基第四系軟土層厚、強度低的現實,結合排土場的堆積工藝,採用地基承載能力分析、邊坡穩定性分析等方法,分析確定了排土場的結構參數,為該排土場的生產提供了依據。
  20. We have also studied fracture formation and moving period by means of growth triangle zone and equilibrium section technology. the result is that fracture formation period in diffirentt struture zone are very d ' rffirent. the basic law is that from the north to the south, the fracture formation period is later and later

    利用生長三角帶和平衡剖面技術對斷裂形成時期和活動時期進行了研究,結果表明,不同構造帶斷裂形成時期存在很大差異,基本規律是從北到南斷裂形成時間越來越晚,但斷裂主要活動時期則在庫車期?第四系
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