planation 中文意思是什麼

planation 解釋
n. 名詞 【地質學；地理學】均夷作用。

  1. The late pleitocene was the essential duration for the planation of the region, when the basic frame - work of the present geomorphology of beijing plain was constructed

    更新世中期本區湖沼廣布。更新世晚期是本區平原化的主要時期。塑造了北京平原現時地貌的基本格架。
  2. According to geologic basement, it can be divided into stable - floor planation surface and active - floor planation surface. according to climate zone, it can be divided into pediment and pediplain, double leveling surfaces and etchplain, peneplain and cryoplain

    夷平面理論研究與初步模擬? ?中文摘要影響夷平面形成的主要因素有前期大地構造、侵蝕基準面、氣候、巖性、時間和後期構造運動等。
  3. We also considered the 3d presentation and analysis of the planation surface

    文章還進行了夷平面三維顯示和分析的初步探討。
  4. The age of planation surface means the end of the planation

    夷平面的年齡就是夷平作用停止的年代，即夷平面開始破壞解體的年齡。
  5. Chronology of planation surface is one of the most important part of the study

    夷平面的測年是夷平面研究中非常重要的一個方面。
  6. This paper ' s main aim is to narrate the technology and the principle of agent planation in two layers of metal process

    摘要本文主要敘述了雙層金屬布線中介質平坦化的工藝及原理。
  7. Different type of planation surface has different formation, the difference of planation results in the difference of planation surface

    不同類型的夷平面有不同的形成過程，夷平作用的差異導致了夷平面類型的差異。
  8. Phase - transition analysis, age - boundary line analysis, correlation and crust of weathering analysis are all used in determining the age of the planation surface

    本文介紹了相過度法、年界法、相關沉積法和風化殼法等測定夷平面年齡的方法。
  9. There are lowering and backing of the ground when it was planated. planation can be classified into many types such as peneplaination, pedimentation, cryoplanation and double leveling surfaces planation

    夷平作用大致可分為準平原化夷平作用、山足夷平作用、凍融夷平作用和雙層水平面夷平作用等幾種類型。
  10. Planation is a combination of external agents. erosion is the primary significance in that it cuts all the strata formed previously and in the combination with transportation and accumulation, directly affects the formation of planation surface

    夷平作用是以侵蝕為先導，輔以搬運、堆積、伴隨有地形的蝕低蝕退，以接近侵蝕基準面為目標的一種外力組合。
  11. Finally, it also discusses the sign ifi cance of thermal fluid flow to pool - forming dynamics ： ( 1 ) provides a new ex planation way to abnormal vitrinite reflectance, which can enlarge the fields of hydrocarbon exploration and development ; ( 2 ) provides some important evidences to research of hydrocarbon migration, which support to choose exploration targ e ts ; and ( 3 ) provides means to study diagnesis and porosity evolution of reservo ir rocks, which can be used to predict the development units of deep reservoir s

    最後，探討了熱流體活動對成藏動力學研究的重要意義，認為其可為有機質演化異常提供新的成因解釋途徑，擴大油氣勘探領域；為油氣運移的研究提供線索，優化勘探目標選擇；為成巖-孔隙演化的動態研究提供依據，預測深部儲層發育層段。
  12. According to whether there are later tectonic activities or not it can be divided into mountain planation surface, lower planation surface and buried planation surface. according to active condition, it can be divided into active surface, dormant surface, exotic surface and defunct surface. taking the base level into consideration, it can be divided into sea - eroded and deposited planation surface, denudated planation surface, snowline planation surface and upper eroded planation surface

    依據夷平面形成后是否遭到後期構造變動將夷平面分為山地夷平面、原地夷平面和埋藏夷平面；依據夷平面的活動狀態可分為活動面、休眠面、外來面和廢止面；依據侵蝕基準面可分為海蝕-堆積夷平面、剝蝕夷平面、雪線夷平面和上部剝蝕夷平面；依據基底可分為穩定地帶上的夷平面和活動地帶上的夷平面；依據氣候帶可分為準平原、山麓面和聯合山麓面、雙層水平面和刻蝕平原、凍融山足面和凍融剝夷平原。
  13. Samples was only 0. 37 which was the smallest among coefficients ; tl, t2, t3 and t4 which came from gaozhuang plantation, mianyang, sichuan, and t5, t6, t7, which came from laohegou planation, mianyang, sichuan, were clustered two groups. the greatly genetic variations in samples of gastrodia elata bl. in different areas and altitude were revealed though the analysis of the tree plot

    從總體上看，采自高莊林場的n ， t2 ， t3 ， t4和老河溝采育場的t5 ， t6 ， t7及采自雅安地區的t9 ， t8可以聚為兩大類，說明由於地理分佈和海拔高度的不同，天麻種內的dna存在較大的變異性。
  14. Original planation surface has some features, for example, it appears in large area with low altitude, small gradient and taking a long formation period, etc. discrimination of planation surface is based on plotting and field investigation and by using statistical methods and " 3s " technique

    原始的夷平面具有分佈面積較大（全流域范圍） 、坡度較小、高度較低、形成所需時間較長、有夷平作用的痕跡等特點。基於野外考察和室內作圖，可利用數學統計方法和「 3s 」技術進行夷平面的識別，這加強了夷平面研究的精確性、客觀性和定量性。
  15. We strengthen the investigation of natural factors such as pre - construction, erosion base level, climate, lithology, time and tectonic activities, which affect formation and preservation of planation surface. pre - constrction affects the time and degree of the planation. erosion base level is the base line for it

    前期大地構造影響夷平面發育的時間和程度；侵蝕基準面是夷平面發育的「終點站」 ；氣候直接和間接作用於夷平面的形成與保存；巖性影響夷平面形成的過程和時間；時間作用於夷平面發育和保存的程度；後期構造不利於夷平面的保存。
  16. The first part discusses the theoretic connotation and historical evolvement of power, taking the ex planation of power in different times and different countries into account, discussing that " serving people " still is the core tenet for leaders and cadres " coming into power under the greatly changed political and economical circumstances. the second part discusses the issue that how to make use of power correctly, discussing the following issues in turn : the impersonal political and economical circumstances of the use of power ; the four factors which often cause the happening of the mistakes of power - using ; the basic demands n principles and requirements of the use of power, and discusses the fundamental measure of the right use of power - - - - - - the establishment of systems, attaching more importance on the system of cadre and person, the system of decision - making of important matters, the system of supervision. at last the thesis discusses the safeguard of the right use of power - - establishment of professional morality of the leaders and cadres

    第一部分通過論述權力的理論概念及歷史演變，結合古今中外人們對權力的不同解釋，論述了我黨在執政環境發生重大變化的今天，領導幹部掌權用權的核心和宗旨依然是「執政為民」 ；第二部分論述了如何正確行使權力的問題，依次論述了權力行使的客觀政治經濟環境，權力得到正確行使的基本要求，導致權力運行失誤的四種經常性因素，以及保障權力得以正確行使的制衡性原則、公開性原則、法制性原則、自製性原則，並以幹部人事制度、重大問題決策制度與監督制度為重點論述了權力得以正確行使的根本? ?制度建設，最後討論了權力得以正確行使的有力保障? ?領導幹部職業道德建設，分別論述了幹部職業道德建設的主要內容及途徑。
  17. This paper probed the theory and modeling on the planation surface through its definition, discrimination, classification, distribution, formation, dating, and so on. we also made 3d presentation and analysis of the planation surface by using photoshop, mapgis and excel

    本文從夷平面的定義和識別、分類及分佈、形成、年齡等幾個方面進行了夷平面理論和實踐的探討，並利用photoshop 、 mapgis 、 excel等對夷平面進行了三維顯示和分析。
  18. Planation surface is a wide - ranging and undulating surface formed by planation in a long and relative stable period or in a decreacing - development period. it is near the base level and there always exists some deposits such as crust of weathering above it. planation surface is often uplifted or buried by the later tectonic activities

    夷平面是在長期的地殼相對穩定時期或地殼下降發展階段，由廣泛的夷平作用以截斷面形式橫切所有先成的地層和構造的接近侵蝕基準面的平緩的地表形態，其上常有風化殼等碎屑堆積，常遭到後期的抬升切割或埋藏，分佈於地球的各緯度帶。
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