氣成期 的英文怎麼說

中文拼音 [qìchéngqī]
氣成期 英文
pneumatolytic stage
  • 氣 : Ⅰ名詞1 （氣體） gas 2 （空氣） air 3 （氣息） breath 4 （自然界冷熱陰晴等現象） weather 5 （氣味...
  • 成 : Ⅰ動詞1 （完成; 成功） accomplish; succeed 2 （成為; 變為） become; turn into 3 （成全） help comp...
  • 期 : 期名詞[書面語]1. （一周年） a full year; anniversary 2. （一整月） a full month
  1. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據沉積學、石油地質學和層序地層學理論，綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料，對鄂爾多斯盆地塔巴廟區塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明，研究區內目的層段可以劃分為2個沉積體系： （ 1 ）上石炭統太原期為有障壁海岸沉積體系，發育潮坪?瀉湖?障壁砂壩沉積。
  2. The causes are discussed from aspects of oil - gas source beds, trapping and storing space, oil - gas migration channel and thick proofing layers, oil - gas maturity stage and allocation of effective trapping stage, suggesting the searching of primary oil - gas pool of the cambrian and lower ordovician at the relatively shallow layers and surrounding places with faults developed

    從油氣源層、圈閉與儲集空間、油氣運移通道與巨厚隔層、油氣成熟期與圈閉有效期配置等四個方面探討了未獲油氣之原因，提示在滿加爾坳陷腹地，相對較淺部位及周邊斷裂發育部位尋找寒武系和下奧陶統的原生油氣藏。
  3. In this paper, thermal evolution history of organic matter of the source rocks and hydrocarbon generation history have been researched by tti method, hydrocarbon migration direction and migration times were probed combining with the area structure development feature ; distribution pattern of the main reservoir intervals on lateral and longitudinal have been predicted by researching on development feature and control factors of the reservoir intervals, the actions of reservoir conditions in hydrocarbon accumulation and bearing also were probed combining with pore evolution feature ; the micro - pore feature of regional cap and direct seal in carboniferous - lower triassic in this area have been determined with micro - capillary pressure curve and intrusive mercury curve ; the prospecting districts have been pointed out combining with the hydro - geologic feature, the potential reservoirs were classified according to trap types in this area, the author attempt to evaluate on the hydrocarbon - bearing condition in the str ata of carboniferous ~ lower triassic from hydrocarbon generation and migration reservoir condition, reserved condition etc, and predict the reservoir types and hydrocarbon - bearing patterns combining with the structure evolution. based on above, the author point out that the central block of chenghu - tuditang synclinorium and the southern block of dangyang synclinorium are the advantageous regions for exploration

    本文用tti方法研究了烴源巖有機質的熱演化史和油氣生成史，並結合區內構造發育特徵，探討油氣在區域上的運移方向和在時間上的運移期次；通過對儲集層段的發育特徵和控制因素的研究，預測了本區主要的儲集層段在橫向上和縱向上的分佈規律，並結合孔隙演化特徵，探討儲集條件在油氣聚集成藏中的作用；利用微毛細管壓力曲線法和壓汞法，對石炭系?下三疊統的區域蓋層和直接蓋層的微孔隙特徵進行了定量評價，並結合水文地質分佈特徵，指出有利於油氣保存的地區；根據區內存在的各種圈閉類型，對可能存在的油氣藏進行了分類，並試圖從油氣的生成與運移、儲集條件、保存條件等方面，動態地綜合評價石炭系?下三疊統油氣成藏條件，並結合構造演化特徵，預測其油氣藏類型和成藏模式。
  4. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演化史綜合方法，確認焉耆盆地侏羅系油氣藏具有三期成藏的特點，第一期發生在侏羅紀晚期，是盆地的主要成藏期，第二期為侏羅紀末至白堊紀的油氣藏破壞、調整和再分配期，第三期發生在第三紀，是盆地的次要成藏期。
  5. According to those analysis and the background of geological evolution of basin, the kind of hydrodynamics was regarded as compaction before y3 and then as compaction - osmosis after y3. futhermore, the key time of oil and gas reservoir formation was summarized, it is furthermore, the main cause of high pressure formation was believed that the compaction was not enough in paleogeothermal gradient, meanwhile, analyzing the cause of the low pressure nowadays, it was the uplift and erosion of stratum or pressure divulgence because of seal and so on

    另外，還確定油氣成藏的關鍵時期為伊敏組沉積末。再者，認為欠壓實是最大埋深狀態下，超壓形成的主要原因，同時分析了形成現今負（低）壓的原因，其原因為地層抬升剝蝕、壓力因封閉層的泄漏等。最後，恢復出各主要目的層的古流體勢的演化歷史，從伊敏組末至現今，油勢分佈特徵具有較好的繼承性。
  6. Detailed studies of tectonic unit and mineralized pedigree in each tectonic unit and each period provided that tectonic evolution passed an evolutionary sequence from early extension - transition - late compression that correspond to mineralization - sediment and submarine eruption - exhalation mineralization - moderate to acid magma and tectonic hydrothermalism that are relevant to mantle - derived magma and volcanic activities ; the mineralized pedigree can be indicated as mantle derived - inner basin and deep source - crust source ore - forming materials

    對各時期、各構造單元的成礦譜系進行了詳細研究，提出構造運動演化從早期拉張過渡晚期擠壓的演化序列，分別對應于以幔源巖漿和火山活動有關的成礦作用沉積及海底噴流?噴氣成礦作用中酸性巖漿及構造熱液成礦作用；在成礦物質上由幔源盆內及深源殼源的成礦譜系。
  7. The structural elements of controlling reservoir forming in kenxi area are studied and estimated systematically, the vertical and plane evolution processes of sedimentary in kenxi area are set forth, time and space spread and its controlling factors of the hydrocarbon source rock and reservoir are analyzed, two types of hydrocarbon source rock ( es3, es4 ), two types of heavy oil, two periods of hydrocarbon generation, two periods of hydrocarbon drain, two stages of reservoir forming and five dynamic systems of reservoir forming are definite in kenxi area

    對墾西地區油氣成藏構造要素進行了綜合地研究評價，闡述了其沉積縱向及平面演化過程，分析了生油層、儲集層時空展布及其控制困素，識別出本區有沙四、沙三兩套油源層，兩種類型的稠油，有兩個生烴期、排烴期、成藏期，五個成藏動力系統。
  8. Analysis of petroleum accumulation phase in dongying sag

    東營凹陷油氣成藏期分析
  9. And the hydrocarbon - generating is mainly from late cretaceous to tertiary, while traps formed mainly from late cretaceous to tertiary, prior to the hydrocarbon migration or simultaneously, with a fine coordination on the duration

    主要生烴階段發生在晚白堊-第三紀，圈閉的主要形成期在晚白堊紀-第三紀，圈閉形成時間基本早於或同時于油氣運移時間，具有較好的時間配套關系。
  10. The first is early period of dongying - guantao, which is the main stage for natural gas forming with erosion and decrease of pressure. the second is from the beginning of quaternary to update, during which gas reservoir is reforming and the reforming gas is refilling into the reservoirs. according to the value k / ar in illite, the time to form the gas reservoirs can be determined as the period of dongying - guantao, among which duzhai is 43. 0 - 38. 0ma and 25. 4ma, qiaokou area 37. 8 - 25. 4ma and 24. 4 - 18. 4ma, baimiao 38. 0 - 25. 4ma and 23. 4 - 20. 4ma

    伊利石測年法確定的天然氣成藏時期主要為東營?館陶組早期，其中杜寨主要為43 . 0 - 38 . 0ma及25 . 4ma ；橋口地區為37 . 8 - 25 . 4ma及24 . 4 - 18 . 4ma ；白廟地區為38 . 0 - 25 . 4ma及23 . 4 - 20 . 4ma ；杜寨地區成藏較早，伊利石測年確定的是天然氣藏最早形成時期，是天然氣藏形成的上限，伊利石測年法確定的天然氣成藏期是兩大主要成藏期的第一階段。
  11. The main task of this article is analysing the major source rock ' s burial history of oil - gas - bearing basin in china and in other countries, and researching different burial history type basin ' s reservoir characteristic, and relationship between the phase of reservoir formation and different burial history type basin. the basic thoughtfulness is firstly analysing the rebuilding burial history theory and ways, then classifing and analysing the source rock ' s burial history of oil - gas bearing basin in china and in other countries, and analysing the reservoir characteristic of different burial history type basin and reservoir formation phase of different burial history type basin

    本文的重點任務是對國內外含油氣盆地主力生油層系的埋藏史曲線進行分析，並研究不同類型埋藏史的盆地油氣藏特徵以及油氣成藏期與埋藏史的關系。基本思路是首先對埋藏史恢復的原理和方法進行分析，然後對國內外含油氣盆地主要生油層系的埋藏史進行歸類與分析，分析不同類型埋藏史盆地油氣藏的特徵，以及埋藏史與成藏期的關系。
  12. Lord may said : " we, the industrialised nations, have an obligation to help developing nations to develop their own solutions to the threats they face from climate change. " notes for editors

    我們使用unfccc關于氣候變化的定義，即：直接或間接地由改變大氣成分的人類活動所導致，並且在比較期觀測到的自然氣候變動的氣候的一個變化。
  13. The paper presented the evolution of five key indicators property prices, property transaction volumes, new mortgages, the income - gearing ratio, and the buy - rent gap, which measures the funding cost of buying a property relative to its rental yield in the form of a pentagon, to compare the current situation with the boom and bust cycles of the past decade or so

    該文件以五邊形的方式闡釋5項主要指標的演變物業價格物業成交量新造按揭貸款收入與供款比率，以及反映購買物業的資金成本相對于租金收益的購入成本與租金差距，以比較目前的情況及過去十多年來的景氣及不景氣周期。
  14. The preface of this paper introduce the increasing new risks which provides the playground to catastrophe insurance securitization. chapter 1 describes the development and theoretical resource of catastrophe insurance securitization. chapter 2 states the increasing catastrophe risks and the challenges to traditional reinsurance, as well as the effects that produced by catastrophe insurance securitization. chapter 3, the main part of this paper, mainly discusses the several insurance derivatives. the main part discusses the several insurance derivatives produced by the securitization of catastrophe insurance : and etc, including the constructures operation advantages and disadvantages and the key factors of the dealing success

    本文的緒論部分介紹了新興風險的不斷涌現及其對巨災保險證券化所提供的背景；第一章介紹了保險證券化的發展及其理論基礎；第二章論述了巨災風險不斷擴大的趨勢下巨災風險對傳統再保險所提出的挑戰和巨災保險證券化對傳統再保險的影響；其主體部分即第三章主要論述了巨災保險證券化所產生的幾種保險衍生型產品：巨災債券、巨災期權、氣候期貨與期權以及其他幾種衍生型產品，包括其結構、運作、優缺點及其交易成功的關鍵因素等方面。
  15. Bozhong area has different oil - gas accumulation characteristics from the adjace nt onshore oil fields. because of the latter thermal event and tectonic action, bo zhong area became the subsidence center and depo - center of the bohai bay basin

    其具有不同於周邊陸地油田的油氣成藏特點，晚期的熱沉降和構造活動使其成為渤海灣盆地的沉降和沉積中心，上第三系具有優于周邊陸地油田的良好的儲蓋條件，晚期的構造活動與油氣主要排烴期相匹配，為油氣向上第三系圈閉中運聚提供了良好條件。
  16. Natural gas in duzhai area was formed the earliest. inclusion enclave temperature testing not only determined the first stage for natural gas formed to be 28 - 20ma but also the second stage to be from quaternary ( 2ma )

    包裹體測溫法不僅確定了第一階段天然氣成藏期為28 - 20ma ，也確定了第二階段天然氣成藏期，即第四紀以來（ 2ma以來） 。
  17. On studying of them. using the testing outcomes of gas fully, lithologic characters. strata sequence, sand body shape, sequence sectional structure in aeration zone and main channels migrating pattern on different phases have been analysed. for futher reservoir, cap, source rock and oil gas expiortion

    在此研究基礎上，充分利用有關的試氣成果資料，詳細分析了含氣層的巖性、層序地層特點、砂體的形態產狀特徵、不同時期主河道分佈與遷移的規律及含氣層的剖面結構特點等。
  18. Study on the pool - forming periods of oil and gas in qijia - gulong sag in songliao basin

    古龍凹陷油氣成藏期次研究
  19. Different weather conditions, such as unreasonable rains at the time of flowering and droughts during harvest and post harvest stages, mould growth and so mycotoxins contamination can also pose serious problems

    此外，天氣出現不尋常的轉變，例如在開花日子暴雨連場，又或在收成期間收割後期出現旱災，黴菌便會不斷繁殖，導致黴菌毒素污染為患。
  20. In different geologic development stage, different geodynamics background and tectonic stress field characteristic led to different baisin types, sedimentary assemblage. basin - mountain coupling forms and produced complex structure deforming. consequently, superimposed basin are characterized by multi - stage basin - formation, multi - stage hydrocarbon generation, multi - stage hydrocarbon accumulation. complex accumulation mode and oil / gas distribution law. tectonic process is key point and decisive in many hydrocarbon accumulation factors of superimposed basin

    在不同的地質發展階段，由於不同的地球動力學背景和構造應力場特徵，導致了不同的盆地類型、沉積組合、邊界條件和盆山耦合形式，產生了復雜的構造變形，從而使疊合盆地具有多期成盆、多期成烴、多期成藏以及復雜的油氣成藏模式和油氣分佈規律。
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