slope evolution 中文意思是什麼

slope evolution 解釋
坡面演進
  • slope : n 1 傾斜,坡度;坡,斜坡,斜面;【印刷】斜體。2 【軍事】掮槍的姿勢。3 【數學】斜率。4 【礦物】斜...
  • evolution : n 1 發展,發育;開展。2 (氣體等的)放出;散出,放出物,散出物。3 發生;演變;【生物學】演化,進...
  1. It is a rather well - known fact that bank - slope deformation and failure result from the coupling of earth ' s endogenic and exogenic geological processes, in which different dynamic - force factor has a different correlation to the evolution of bank - slope

    摘要河谷岸坡的變形與破壞是地球內外動力耦合作用的結果,並且每一種動力地質作用對于岸坡變形失穩的貢獻程度不同,造成岸坡變形破壞頻率和規模的空間差異。
  2. The gullies are formed by the processes of infiltration - interflow - collapses. ( 2 ) in the slope with sand - loess, the major factors of water erosion are the rainfall intensity and rainfall amount of annual first rainfall. ( 3 ) in the region, the evolution processes of slope gully system results from alternative actions of sand deposition and water erosion

    ( 1 )有片沙覆蓋的斜坡小區,徑流量少,但徑流含沙率大,坡溝的形成過程是:垂直滲流坡地潛流崩塌; ( 2 )在沙黃土斜坡小區,每年春末夏初降雨的強度及降雨量是決定坡面產沙量的關鍵因素; ( 3 )該區坡溝系統的形成發育是風沙沉積、風蝕與水蝕交替作用的結果。
  3. Using the variational method, analytical conditions for stationary pulse propagation in dense period fibers with strong dispersion management are deduced. the expression of initial soliton peak power is given. by employing the obtained formulas, the soliton evolution semi - analytically in various dispersion maps can be investigated. effects of the third order dispersion are also studied in this paper. the results show that imperfect dispersion slope compensation can cause pulse central position shift and even serious degradation of soliton shape

    利用變分方法,推導出了在強色散管理的密集周期光纖中脈沖穩態傳輸的解析條件,並給出了初始脈沖峰值功率的表達式.運用這些公式,對各種色散管理系統中孤子的演化進行了半解析的考察.三階色散也被考慮在內.結果表明:不完善的色散斜率補償將導致脈沖中心位置的偏移甚至嚴重的孤子形狀劣化
  4. Diagenesis and pore evolution of submarine fan reservoir in the west of northern steep slope, dongying sag

    東營凹陷北部陡坡帶西段水下扇儲層成巖作用與孔隙演化
  5. The judgement formula for high and low speed landslide and a new theory of stiffness - effect instability are presented for the instability of planar - sliding slope by the catastrophe theory. it is pointed out that the limit equilibrium stability analysis method of rigidity body has a lot of defects. the relationship between the action of outside environment and the response of slope system is complicatedly nonlinear according to the nonlinear dynamics model of slope evolution built

    針對斜坡平面滑動失穩問題,運用突變理論方法,給出了快速滑坡和慢速滑坡發生的判據,驗證了剛體極限平衡穩定性評價方法有較大缺陷;根據斜坡演化非線性動力學模型,發現斜坡演化過程會出現混沌現象,其通向混沌之路是通過倍周期分叉實現的。
  6. In order to furtherly study the petroleum accumulation law, this paper, based on the tectonic evolution, started from main hydrocarbon generation periods of the main resource rock, analysed petroleum generation, migration, accumulation, adjustment and dynamic accumulation process. according to area structural characteristic, bachu - markit was divided into the three sub - structure unit, that is, east part of bachu arch, west part of bachu arch and markit slope and established accumulation model of each part

    為了更深入的分析油氣聚集規律,本論文從主力烴源巖的主生油期出發,避開細枝末節,以區域構造演化為線索,分析油氣生成,運移,聚集,破壞調整,再次運聚成藏的動態過程。根據巴楚?麥蓋提地區的區域構造特點,將該區分為三個次級構造單元,即巴楚隆起西段、巴楚隆起東段、麥蓋提斜坡,分別建立了成藏模式。
  7. However, the true reason that markit slope are so steep is due to intense tectonic movement of late himalayan. as concerned as this hydrocarbon source regional evolution, the key tectonic movements for hydrocarbon accumulation can be divided into three stage : ( 1 ) middle - late caledonian movement ; ( 2 ) late - terminal hercynian movement ( 3 ) late himalayan movement

    給合本區的烴源巖演化史,對本區油氣運聚成藏關鍵性的構造運動有三期:中晚奧陶的伽里東中晚期運動;早晚二疊的海西晚、末期運動喜馬拉雅晚期。
  8. As the evolution process of the drainage channels on the scarp slope is concerned, the construction of their mathematic models and the visualization methods are discussed

    對斷層崖上的溝谷演化過程,我們也對其數學模型的構造和可視化方法進行了探討。
  9. Numerical modeling on seepage in side slope based on immune evolution algorithm

    基於免疫進化規劃演算法的邊坡巖體滲流數值模擬
  10. The main thrust of this study are follows : the primary study provides in detail the area structural properties including the fault systems, structure units, and trap types ; the secondary study including the sedimentary systems including stratigraphic classifications, depositional environment properties, infilling - evolution properties, and oil source analysis ; the third area of study including the geologic property of the north slope zone ; and the final area of study provides an analysis of gas and oil accumulation, the types and distribution of reservoirs, and the pool - forming models used

    本研究主要從事了以下工作,較為詳細地研究了該地區斷裂體系、構造單元、圈閉類型等構造特徵;從地層劃分、沉積特徵、沉積環境、充填演化特徵、油源分析等方面研究了該地區的沉積體系;詳細地研究了油氣資源豐富的北部緩坡階梯帶的地質特徵;根據成藏動力學系統理論,較為詳細地研究了該區的油氣運聚模式、油氣藏類型及油氣藏分佈規律。
  11. The research method of combining the structural evolution with hydrocarbon accumulation has important directive function for oil & gas exploration in kongquehe slope of tarim basin

    摘要構造演化與油氣成藏相結合的研究方法,對于塔里木孔雀河斜坡的油氣勘探具有重要的指導意義。
  12. Basin - range evolution and oil - gas exploration in altun slope area of western qaidam basin

    柴達木盆地西部阿爾金斜坡地區盆山演化與油氣勘探
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