巖生 的英文怎麼說

中文拼音 [yánshēng]
巖生 英文
iwao
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 生 : Ⅰ動詞1 （生育; 生殖） give birth to; bear 2 （出生） be born 3 （生長） grow 4 （生存; 活） live;...
  1. Sulfid also can be regarded as a marker of the action of sulfur bacteria. 8 ) based on research results, author postulated that early generation of hydrocarbons is closely related to the action of sulfur bacteria. many kind of algae such as dinoflagellates, diatom, prynesiophytes etc have rich biological lipids which has lower polymerization

    6 、從未熟一低熟源巖生烴組分及其演化、可溶有機質轉化生烴等方面，探討了未熟一低熟油的形成機制，提出本區未熟一低熟油氣的形成是低活化能的富氫腐泥組分受到硫細菌早期低溫降解作用的結果。
  2. At last, based on the results of geologic history numerical simulation and the force and substance balance theories of deep basin gas, the dynamic procedure of the entrapment forming of reservoir, the characteristics of generation and discharge gas of the source rocks and the coupling relations between the two are studied, so the distribution and the reserves of deep basin gas at specific geologic times have been obtained

    結合深盆氣藏的力平衡和物質平衡理論，研究了儲層形成圈閉的動態過程、源巖生排烴特徵、以及二者之間的耦合關系，得到了小草湖窪陷不同地史時期深盆氣藏的分佈范圍和儲量。
  3. A sere on uncovered rock is a lithosere.

    在光禿巖石上的演替系列是巖生演替系列。
  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. The essential elements and process of gas reservoir formation of ordovician in ordos basin have been annalysed systematicly and scientificly by means of the theory and method of organic geochemistry and tectonic geology in this dissertation. the several advanced techniques, such as gas generation thermal simulation, on - line individual gas compounds carbon isotope determination ( py - gc - c - ir - ms ), the analysis technique of light hydrocarbons and biomarkers in natural gas, gas migration simulation and gas carbon isotope determination in fluid inclusions, have been applied to focuse on the study of the gas generation mechanism of souce rock, correlation between gas and source rock, reservoir formation history, migration direction, charging road in detail

    應用有機地球化學和構造地質學理論和方法對鄂爾多斯盆地奧陶系天然氣地質研究中薄弱環節成藏要素和作用進行了系統科學分析。利用烴源巖生氣定量熱模擬技術、熱模擬在線碳同位素實驗技術、氣體輕烴和生物標志物分析技術、運聚成藏物理模擬技術和包裹體中碳同位素分析技術等多種先進的實驗技術對烴源巖的生氣機理、氣源和混合比、成藏史、充注路徑、運移方向和構造作用與成藏關系等問題進行了深入的研究，在前人研究的基礎上，經過本次大量的實驗分析和綜合研究，提出了一些新的認識。
  6. 7. the source rock in de nan depression has the characteristics of a short period of expulsion, early tectonic ceasing, short migration distance, therefore ; the most favorable places for entrapment is near oil kitchen and on the pathways of migration

    7 、德南窪陷低熟油灶具源巖生排烴期短、構造定型早、鍋底生油、油氣運移不遠等特點，故近源、在運移路徑上的圈閉是形成油氣藏的有利地區。
  7. The main process of hydrocarbon generation and expulsion in es3 hydrocarbon - bearing rock began in the late of ed epoch and ended in ng epoch ( equals to 30 - 12ma ). the generation and expulsion of oil of es1 epoch began in nm ? epoch and ended by the deposition of quaternary system ( equals to 10 - 5ma ) and reached its peak after the deposition of nm epoch

    3 、歧口凹陷主要烴源巖生排烴史的研究確定了門限深度和生排烴時間，沙三段源巖的主要生排烴作用過程是在東營末期至館陶期完成的（相當於30 ? 12ma ） 。
  8. Much work has been done on the hydrocarbon generation patterns of source rocks from the dongying depression based on laboratory thermal simulation experiments, but there is no report on ki netics of hydrocarbon generation of the source rocks

    採用乾酪根生烴動力學參數外推地質過程近年來，在國外受到高度重視，在國內也開始了這項工作，取得了較好應用效果。東營凹陷烴源巖生烴作用的熱模擬實驗已做大量研究工作。
  9. In himalaya period, the basin was compressed. as tertiary deposits increased, jurassic source rocks started secondary hydrocarbon generation, thus resulting in the activation and reconstruction of the petroleum system

    燕山運動中晚期，侏羅系大規模沖隆及剝蝕，侏羅系源巖生烴作用終止，含油氣系統被破壞。
  10. Based on the hydrocarbon - generation models of the source rocks from this study, an improving method to calculate petroleum - generating amounts and petroleum resource amounts has been suggested

    並在此基礎上，對牛莊窪陷南斜坡es _ 4頁巖生油量與油氣資源量進行了評價。
  11. Some conclusions have been made in the following. that the value of toc is 0. 2 % may be regarded the low evaluation value of marine carbonate souce rock at the stage of high to over mature. according to the content of bitumen in source rock and reservoir, gas generation quantity, the maximum absorption gas quantity and geology analogy

    通過對儲層和烴源巖中瀝青定量統計分析、烴源巖生氣熱模擬、最大吸附氣實驗測定及地質類比法等綜合研究認為在鄂爾多斯盆地有機碳為0 . 2可作為高?過成熟的海相碳酸鹽巖有機碳下限標準。
  12. This study used some techniques such as organic geochemistry bulk composition combined with molecular geochemistry, source rock analysis and evaluation of organic petrology, carbon isotopes of organic matter, petroleum geology inference etc. the emphasis is mainly concentrated on the source rocks belong to the shahejie formation of pal eocene, including the source rock evaluation of denan region, geochemistry of the source rock, biomarkers of immature oils and source rocks. then the ancient geological environment was established and immature oil formation mechanism was proposed. following results have been tentatively proposed in this thesis : 1 ) based on the organic petrology studies, most of source rocks in this region is belong to immature source rock

    本項研究以德南窪陷重點烴源巖- - -下第三系沙河街組為對象，應用有機地球化學理論與方法對其有機質類型和豐度、成熟度、生烴潛量等進行研究；通過特徵生物標志化合物的分析，闡明研究區未熟-低熟烴源巖母質構成、沉積環境和成熟演化；通過油源對比和生烴條件綜合分析，提出本區烴源巖生烴機制，建立未熟-低熟烴源巖有機質生烴模式。
  13. Unfortunately most of researches on this issue were concentrated on conformation and classification, few studies on acclimatization mechanism and corresponding ecology and nutrition characteristics were reported. in this study, we chose puyuan village of bishan county, laifeng town, backhill of southwest agricultural university, and jingyun mountain as research sites

    金發草是極其重要的植被恢復巖生植物，目前國內外對其多集中在形態、分類的報道上，而對金發草適生環境理化性質、水分特徵以及其與環境相適應的生態特徵、營養特性的研究罕見。
  14. However most researches on rock plants both at home and abroad emphasized their individual characteristic, their acclimatization mechanism and great ecological potential were neglected. therefore, ecology and nutrition characteristics, as well as drought resistance mechanism of rock plants were poorly understood. as an important rock plant, pogonatherum paniceum ( lam. ) hack

    然而，國內外對巖生植物的研究和利用多從宏觀尺度上偏重於其獨特個體特徵，忽略了其內在環境適應機制和巨大生態潛能，缺乏對巖生植物生態特徵、營養特性及其耐旱機理的綜合研究。
  15. On sunday night national nine news broadcast a report about a man who came up with an idea to lace sydney rock oysters with viagra and sell them as souped up aphrodisiacs

    上周日澳大利亞第九新聞頻道報道了一名海產品銷售商創意用偉哥搭配雪梨巖生蠔，並將之作為壯陽藥出售。
  16. From the research on the history of gas formation, caprock sealing and the history of depression activitv, we analvzed the formation and evolution character of gas accumulation systems. then we discussed its controlling effect on the gas deposit formation

    通過源巖生氣史，蓋層封閉史和斷裂活動史研究，分析了天然氣成藏系統的形成與演化特徵，從而探討了其對深層天然氣運聚成藏的控製作用。
  17. Using the angle between orientation of maximum principal compressive stress and strike of source - faults, the vertical seal and open features of source - faults in the end of yimin stage sedimentary period ( the main oil gas accumulation period ) are studied, showing that the source faults in the central area are poorly sealed and well opened in vertical direction and ant the main migration pathway of oil gas generating and expelling from the source rock of nantun formation

    利用最大主應力方向與源斷裂走向之間夾角大小，對貝爾凹陷布達特群源斷裂在主要成藏期伊敏組沉積末期的垂向封閉與開啟性進行了研究，得到了貝爾凹陷布達特群源斷裂在凹陷中部垂向封閉性差，開啟程度高，是南屯組源巖生成排出油氣向布達特群運移的主要輸導通道這一認識。
  18. Investigation into the hydrocarbon generation kinetics of tertiary source rocks from the west of qaidam basin

    柴達木盆地西部第三系烴源巖生烴動力學研究
  19. Because the surface source rock are high thermal evolution and low residual organic matter abundance, based on correcting the organic matter abundance pyrolysis loss and surface weathering loss, the authors estimate the hydrocarbon - generation intensity of source rock using the monte carlo technique

    針對地表烴源巖樣品具有高熱演化、低豐度的地化特徵，在有機質豐度的熱解損失和地表風化損失校正基礎上，採用蒙特卡羅法模擬計算烴源巖生烴強度。
  20. The features of secondary hydrocarbon generation of organic matter in coal measures of upper paleozoic in jiyang area

    以鄂爾多斯烴源巖生烴動力學研究為例
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