氣源巖 的英文怎麼說

中文拼音 [qìyuányán]
氣源巖 英文
gas source rock
  • 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...
  • 源 : 名詞1. （水流起頭的地方） source （of a river）; fountainhead 2. （來源） source; cause 3. （姓氏） a surname
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  1. Coal, carbargilite in permo - carboniferous and carbonate in ordovician system were the main source rock of natural gas in the researched area

    石炭二疊系分佈的煤層、炭質泥巖和奧陶系碳酸鹽巖是研究區主要的氣源巖。
  2. Distribution and burying characteristics of the permo - carboniferous system and the coal - formed gas source rock in jiyang depression

    濟陽坳陷石炭二疊系埋藏條件及煤型氣源巖分佈特徵
  3. 1. put forward a new research approach which uses the principle of material balance as the theoretical basis, and quantificationally make grading estimation of carbonate gas source rocks by the quantity of hydrocarbon expelling

    提出以物質平衡原理為理論基礎，以排氣態烴量的有無和大小來對碳酸鹽巖氣源巖進行定量計算分級評價的研究思路。
  4. 3. set up grading estimating criterion of gas source rocks with the gas hydrocarbon expelling intension. figure out the corresponding organic carbon content threshold value, and plot grading estimating plates of oil and gas carbonate source rocks in tarim basin

    基於排氣強度的大小確定了氣源巖分級評價標準，並計算了相應的有機質豐度界限值，繪制了塔里木盆地碳酸鹽巖氣源巖有機質豐度分級評價圖版。
  5. Using maximal diffusive flux to substitute actual diffusive flux, which will overestimate diffusion losing and bring biggish error for estimate of gas source rocks and resource evaluation of gas pool. 5

    以往用最大擴散氣量來代替實際擴散氣量的演算法會過高的估計天然氣的擴散損失量，給氣源巖評價和氣藏的資源評價帶來較大的誤差。
  6. The main achievements are : i. the main gas source rock in xujiaweizi depression is deep color shale of k ^ ^

    論文主要成果及認識有： 1徐家圍子斷陷主要氣源巖為沙河子組營城組暗色泥巖。
  7. In china, most of carbonate source rocks are low organic enrichment and high - maturity, over - maturity, therefore, neither does the existing assessment method of argillaceous gas source rocks in china fit for the evaluation of this sort of source rocks, nor can copy the foreign evaluation of lower maturity carbonate gas source rocks. the value of carbonate gas source rocks is an important thing that determines the investment and oriention of exploration

    我國碳酸鹽巖普遍有機質豐度低且以高過成熟為主，對其氣源巖的評價不僅不適宜直接採用國內已有泥質氣源巖的評價方法，也不能照搬國外較低成熟度碳酸鹽巖氣源巖的評價方法，然而，對氣源巖的評價事關我國對天然氣的勘探方向和投資力度，因而具有極其重要的現實意義。
  8. Most of carbonate source rocks in our country are high - maturity, over - maturity, therefore, neither does the existing assessment method of argillaceous source rocks in china fit for the evaluation of this sort of source rocks, nor can copy the foreign evaluation of lower maturity carbonate source rocks

    我國碳酸鹽巖烴源巖以高過成熟為主，這類烴源巖評價（尤其是氣源巖評價）不僅不適宜直接採用國內已有泥質烴源巖的評價方法，也不能照搬國外較低成熟度碳酸鹽巖烴源巖的評價方法。
  9. The distribution of non - structural gas reservoir is constrained by hydrocarbon generating depression and the distribution of high efficient reservoir, the non - structural gas reservoir is often located in a coincident position of the high efficient reservoir and in the crossover of uplift with depression

    非構造氣藏分佈受生烴坳陷和高效儲集層分佈制約，常位於氣源巖與高效儲集層的疊合部位、隆起與坳陷的轉換部位。
  10. Study oil source rocks and gas source rocks respectively

    將油源巖、氣源巖分別加以考慮。
  11. This paper take the conditions of tarim as an example, calculate quantity of gas generation, residual gas hydrocarbon, gas adsorption, gas dissolving in oil, gas dissolving in water, and gas diffusion under different geologic conditions, then according to the principle of material balance, work out gas expelling quantity

    本文以塔里木盆地地質參數為例，計算了不同地質條件下氣源巖的生氣量、殘留氣態烴量、吸附氣量、油溶氣量、水溶氣量、擴散氣量，進而根據物質平衡法計算出排排氣量。
  12. Since the generated gas from gas source rocks is expelled in the form of separate phase, can it be useful for the form of pool. so, the expelling gas value of carbonate gas source rocks is more important, this paper, based on the principle of material balance, divide the tough problem of expelling hydrocarbon into relatively and easily investigated problems of gas hydrocarbon generation, residual and diffusion gas hydrocarbon and evaluate gas source rocks in temis of the magnitude of expelling gas ; hydrocarbon ( quantity of expelling gas = gas quantity of generation - adsorption - dissolving in oil - dissolving in water - diffusion )

    由於所生成的氣態烴只有從源巖中以游離相運移出來之後才能對氣藏的形成做出貢獻，因此對氣源巖的排氣能力的評價顯得猶為關鍵。本文根據物質平衡法原理將比較棘手的排氣態烴問題，分解成相對較易考察的生氣態烴問題和殘留、耗散氣態烴的問題，以排氣量大小（排氣量=生氣量?吸附氣量?油溶氣量?水溶氣量?擴散氣量）為評價碳酸鹽巖氣源巖標準。
  13. Characterization of source rock of shallow tight sand gas in dongliang district in the fuxin basin

    阜新盆地東梁區淺層緻密砂巖氣氣源巖特徵
  14. 6. according to the results of calculation, discuss the effect factor of threshold value of of organic enrichment

    根據計算結果對碳酸鹽巖氣源巖有機質豐度下限的影響因素進行探討。
  15. Take tarim basin as an example to establish theoretical, industrial threshold value of organic enrichment of carbonate gas source rocks

    以塔里木盆地為例建立了碳酸鹽巖氣源巖理論下限和工業下限評價標準。
  16. Through anasynthesis, sum up organic enrichment grading estimating standard of oil source rocks and gas source rocks in our country ( type ii organic matter, mature carbonate rocks )

    經過分析綜合，歸納出我國碳酸鹽巖沉積區（型有機質，成熟碳酸鹽巖）氣源巖有機質豐度分級評價標準。
  17. These source rocks are good gas source rocks and have a certain extent of oil - generating capability based on high abundance and type 2 - of organic matters

    石炭系烴源巖有機質豐度較高，有機質類型以型和2型?主，絕大部分處于生油高峰至干氣期， ?良好的氣源巖，並具有一定數量的生油能力。
  18. As a result, establish the evaluation criterion of source rocks on the basis of quantitative calculation, instead of pure experience, then estimate oil source rocks and gas source rocks respectively

    使對烴源巖評價標準的確定從依靠純經驗過渡到依據定量計算，同時將油源巖、氣源巖分開來進行評價。
  19. Systematically investigate the hydrocarbon generation of organic matter ( oil and gas generation from organic matter and oil to gas ), residual hydrocarbon of source rocks ( residual liquid hydrocarbon of rocks, gas adsorption of rocks, gas dissolving in oil and gas dissolving in water ) and gas diffusion etc. take the conditions of tarim as an example, calculate quantity of oil and gas generation, residual liquid hydrocarbon, gas adsorption, gas dissolving in oil, gas dissolving in water, and gas diffusion under different geologic conditions, then according to the principle of material balance, work out oil expelling and gas expelling quantity

    對評價中遇到的有機質生烴（有機質成油、成氣、油成氣） 、源巖殘留烴（巖石殘留液態烴、巖石吸附天然氣、油溶氣、水溶氣） 、天然氣擴散等問題進行了較為系統的研究，並以塔里木盆地地質參數為例，計算了不同地質條件下烴源巖的生油氣量、殘留液態烴量、吸附氣量、油溶氣量、水溶氣量、擴散氣量，進而根據物質平衡法計算出排油量、排氣量。
  20. The evaluation of oil source rocks is based on magnitude of the expelling oil ( expelling oil quantity = net oil quantity - residual oil quantity ), and the evaluation of gas source rocks is based on magnitude of expelling gas ( quantity of expelling gas = gas quantity of generation - adsorption - dissolving in oil - dissolving in water - diffusion )

    油源巖評價以排油量大小為標準（排油量=凈油量-殘留油量） ，氣源巖以排氣量大小為標準（排氣量=生氣量-吸附氣量-油溶氣量-水溶氣量-擴散氣量） 。
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