gas source rock 中文意思是什麼

gas source rock 解釋
氣源巖
  • gas : n （pl gases ）1 氣，氣體，氣態 〈cf fluid; solid〉 2 可燃氣，煤氣，沼氣；【礦物】瓦斯。3 【軍事...
  • source : n 1 源頭，水源，源泉。2 根源，本源；來源。3 原因；出處；原始資料。4 提供消息的人。5 血統。vt 〈美...
  • rock : n 1 巖，巖石，磐石，巖壁；卵石；〈常 pl 〉〈美口〉石子兒；暗礁，巖礁。2 〈the R 〉直布羅陀 （Gibr...
  1. The thickening may be synthetically aroused by many factors, because of the lower maturation of source rock at forepart, the rock tar is thicker, and then many other factors impel it, which include the hydrocarbon dissipation at the process of oil and gas migration, biodegradation and bathing oxidation induced by gravity induced centripetal flow recharged by meteoric water at the basin uplift period and etc

    稠油成藏則由多因素綜合作用造成，由於早期源巖成熟度較低，原油本身較稠，而油氣運移過程中輕質組分散失、生物降解和盆地抬升剝蝕階段大氣水下滲所導致的水洗氧化等作用則使其進一步稠化。
  2. In qiaokou area, deep parts of well qiaol4, 20, 23, 25, 60 are related to source rock in gegangji sag, while crude oil in well qiao38 is related to source rock in qianliyuan sag ; in baimiao structure, crude oil in well bail2 is related to source rock of es33 - es34 in qianliyuan sag, while condensate in well bai54, 17, 9 is related to source rock of es32 in qianliyuan sag and crude oil in well bai6 is from oil kitchen gegangji. the study on illite age testing, inclusion enclave temperature testing and saturation pressure testing has been used to know the time of the deeply buried gas net pay formed. the time of the deeply buried gas net pay formed can be divided into two stages

    油源對比結果表明杜寨地區濮深15井的凝析油來源於本區es _ 3 ~ 3 es _ 3 ~ 4地層，前8井es _ 3 ~ 2原油來源es _ 3 ~ 2地層；橋口地區東翼葛崗集窪陷一側的橋14 、 20 、 23 、 25 、 60井深層油氣與葛崗集窪陷烴源巖有關，橋口壘塊橋38井原油與前梨園窪陷烴源巖有關；白廟構造翼部白12井原油主要與前梨園窪陷es _ 3 ~ 3 es _ 3 ~ 4段烴源巖有關，構造腰部白54 、 17 、 9等井的凝析油與前梨園窪陷es _ 3 ~ 2段烴源巖有關，白16井原油來源於葛崗集生油窪陷。
  3. 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。
  4. 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。
  5. This is the other main reason for the overpressure in kuche depression to be preserved. we analyzed the effect of fracture in the gas deposit formation and hold that different kinds of fracture have different effect : hydrocarbon dissipation and relief effect of crossing salt bed faults that run through source rock, reservoir, and caprock ; filling effect of under salt bed faults that run through source rock and reservoir ; slippage faults that did not connect source rock have no effect to hydrocarbon accumulation and dissipation ; adjusting faults in reservoir have effect of adjusting formations for hydrocarbon distribution

    分析了斷裂在天然氣成藏中的作用，認為不同類型的斷裂在天然氣成藏過程中的作用是不同的：貫通生、儲、蓋層的穿鹽斷層對油氣散失和泄壓作用；貫通源巖和儲層的鹽下斷層對抽氣運聚的充注作用；不連接源巖的滑脫斷層對油氣聚散無作用；儲層內調整斷層對油氣分佈起調整層位作用。
  6. Based on the study of oil and gas origin, source rock maturation and hydrocarbons expulsion history as well as structural development history, oil and gas reservoirs " formation timing is studied

    陸梁地區的天然氣大致可分為兩類，埋深小於1500n的生物氣或生物氣hb溫熱解氣和埋深大於1500 。的油型氣。
  7. Because of the above mentioned reasons, the first one should be considered the main source rock in yili basin. by means of the modeling of the buried history and the history of thermal evolution, it can be concluded that this set of source rock had entered the ceiling of the oil - generating window in the early triassic period and reached its peek in the middle and end of triassic period, befor entering the highest maturity in the early and middle jurassic period, and had generating gas in the end of jurassic period

    其中鐵木里克組烴源巖厚度大、有機質豐度高、成熟度高，具有較高的生烴潛力，是伊犁盆地主要的烴源巖系，通過埋藏史及熱演化史模擬，該套烴源巖於三疊紀早期已進入生烴門限，中晚三疊世達到生、排烴高峰，早中侏羅世進入高成熟階段，侏羅紀末進入生氣階段。
  8. This difference is caused not only by maturity but also by source rock. natural gas in baimiao area is mainly derived from tertiary source rock and carboniferous permian formation in qianliyuan sag, which is near the high point on lanliao fracture belt

    白廟地區天然氣主要來源於前梨園窪陷第三系烴源巖和石炭?二疊系煤系地層，靠近蘭聊斷裂帶構造高點，淺層es _ 2 ~下? es _ 3 ~ 2氣層具有較高的ar ~ （ 40 ） ar ~ （ 36 ）比值，為煤型氣及混合氣。
  9. 5. platform trough and basin with deep water and low energy are the favorable source rock zones, reef banks and reef cores are the profitable reservoir. and the strata which is dolomitized is the main gas yielding parts

    5深水低能沉積的臺溝、盆地相是有利的生油巖相帶，淺水高能的礁灘、礁核相是有利的儲層，產氣段主要是生物礁內的白雲巖段。
  10. 4. based on the research of geochemical characters of hydrocarbon source rock and comparison of oil and gas sources, it is indicated that the condensed oil and gas in buried hills mainly came from es3 effective hydrocarbon source rock of type iii kerogen - type ii2 kerogen in banqiao deprssion and qikou depression beside both sides of the tilting horst, and which is the main source of buried hill with early reservoir and late oil and gas source

    4根據烴源巖地球化學特徵和油氣源對比，指出潛山凝析油氣主要來自翹傾地壘塊兩側板橋和歧口凹陷的沙三段腐植-偏腐植型有效烴源巖，該凝析油氣是「新生古儲」型潛山的主要油氣源。
  11. ( 2 ) analysis for the forming conditions of hydrocarbon pool, structure and reservoir features shows that the sidaogou structure had two period of migration and accumulation of oil and gas. the first period of migration and accumulation came from the hydrocarbon formed in the source rock of the sanpu depression and formed the asphalt in the sandstone reservoir of triassic and jurassic in the well ha - 2. the second period came from the hydrocarbon formed in the source rock of triassic round about the well ha - 2 and ha - 3 and formed the hydrocarbon pool in the sidaogou

    這是對油藏描述技術和應用領域的完善與補充。通過對四道溝油氣藏油氣源和油氣運移與聚集研究，首次提出四道溝構造存在兩期油氣運移與聚集，指出了油氣生成與運移時期和主運移方向，以及各期油氣對四道溝現今油氣藏的貢獻大小。
  12. According to the chemical experimental data of residual organic carbon content, kerogen carbon isotope, aliphaltic gas chromatography mass spectrometry of 67 outcrop specimens in the baise basin, the authors analyse the geochemical characteristics of the type and the maturation of organic matter in the lower triassic - devonian source rock

    根據百色盆地周緣大量露頭樣品的殘余有機碳含量、乾酪根碳同位素、飽和烴色譜及色質等地球化學實驗數據，分析了下三疊統泥盆系海相烴源巖的有機質豐度、類型、熱演化程度。
  13. 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
  14. 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。
  15. Abstract : the authors studied a lot of related data and analyzed three development stages of the softwares, and it is held that the softwares have the development tendency as follows : ( 1 ) the establishment of model will be based on the space distribution relation of source rock and oil reservoir, it is because the formation of oil and gas reservoir depends on the space relation, and oil reservoir simulation will be combined with oil and gas resource evaluation ; ( 2 ) 3d dynamic simulation will be applied in the simulation of oil and gas migration

    文摘:為了準確和定量地重建出盆地發展過程或油氣成藏過程，掌握盆地與油氣成藏模擬軟體發展趨勢及技術難點，通過研究相關資料，對盆地與油氣成藏模擬軟體的三個發展階段進行了分析.總結出盆地與油氣成藏模擬軟體的發展趨勢：源巖與油氣藏在空間上的關系決定著油氣藏形成過程，應以源巖與油氣藏的空間組合關系為基礎建立模型，將盆地模擬技術與資源評價思想結合模擬出油氣藏形成過程；發展模擬的真三維技術，實現油氣運移的三維動態模擬
  16. Futhermore, the formation of reservoir experienced four periods : the first, from esi to ed ; the second, from late ng to early nm ; the third, nm ; the fourth, from late nm to now. so we predict that exploration in qianmiqiao should be mainly directed to condensed oil and gas reservoir nearby banqiao depression and gas reservoir is more probably found near qikou depression. 8. analogue of the conditions required for reservoir formation in huanghua buried hills shows that, high quality and thick es3 hydrocarbon source rock distributed richly in the middle area depression, and moderate quality sandstone distributed in south area, but the match bet

    8對黃驊坳陷區「新生古儲」型潛山成藏條件的類比分析表明，中區凹陷中分佈有厚度較大的優質沙三段烴源巖，南區分佈有較好的孔二段烴源巖，但中區千米橋地區生儲配置比南區好，因此，整體上中區千米橋潛山一帶油氣藏的勘探前景優于南區。
  17. 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。
  18. 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。
  19. 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
  20. On the basis of above experiments, the chemical kinetic model inwhich organic matter of source rock of deep - formation in the north of songliao basin primarily crack into oil or gas is established, which set up a basis for evaluating oil - generating amount, gas - generating amount of source rock of deep formation in different periods ; set up the chemical kinetic model inwhich different qualities of oil and family constituents in oil secondarily cracked into gas, which provide theoretical foundation and practical methods for dynamic evaluation of gas - generating amount and oil - consuming amount in process of oil cracking. the geochemical features of source rocks in deep - formation of basins are systematically evaluated

    在上述實驗基礎上，建立了松遼盆地北部深層源巖有機質初次裂解成油、成氣的化學動力學模型，為評價深層源巖于不同時期的生油量、生氣量奠定了基礎；建立了不同性質原油及原油中各族組分二次裂解成氣的化學動力學模型，為動態評價油裂解過程的成氣量和耗油量提供了理論依據和實用方法；對盆地深層源巖的地化特徵進行了系統評價；考慮到深層源巖的成熟度較高，實測地化指標（殘余有機碳、氫指數等）不能客觀反映源巖有機質的原始豐度和原始生烴潛力。
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