oil source rock 中文意思是什麼

oil source rock 解釋
生油巖
  • oil : n 1 油；油類；油狀物〈一般是不可數名詞，表示種類時則用 pl 如：vegetable and animal oils 植物油和...
  • 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. 5. the fractures of marlite, sandstone, faults and the disconformity between sha san member and sha er member are three main conduit systems. for this low maturity of the oil kitchen, the fractures of marlite that coexist with source rock might as well be an important bridge to link oil kitchen and reservoir

    5 、通過對德南窪陷輸導體空間分佈及物性特徵分析，揭示並論證了本區特殊的輸導層主要是與源巖共生的泥灰巖、泥質白雲巖及白雲巖中的裂縫系統，為進一步尋找有關油氣藏指出方向。
  2. The oil shale in the lower chang7 oil - bed was the main source rock of oil in the researched area

    長7下部的張家灘油頁巖是研究區主要的烴源巖。
  3. 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。
  4. 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。
  5. In combination with the source characteristics, the three oil groups can be extrapolated to three end - member oils, or three oil populations : population a derived from wenchang source rock, population b derived from enping formation with absence of 4 - methylsterane, and population c might be sourced from the wenchang source rocks in the leftover sags with lowest maturity as a typical feature

    結合源巖分子組成特徵，上述三類原油可被外延至三類端員油： a類端員油，來于文昌組源巖； b類端員油，來于恩平組源巖； c類端員油，可能來于殘留窪陷文昌組源巖。
  6. By the present time, geologic researchers have found that light oil distribute centrally in baier depression. this paper applies this method for identifying and evaluating light oil in the haila ' er basin, and analyzes generation, migration, and preserving condition pramarily. the author thinks that the nonuniform distribution of light oil in haila ' er basin is caused by the difference of distribution of hydrocarbon source rock, type of organic matter which produced oil, tectonic conditions, migrating time, hydrocarbon maturity, and buried depth

    到目前為止，發現海拉爾盆地的輕質油集中分佈在貝爾凹陷，本文舉例說明了輕質油識別理論在海拉爾盆地的實際應用，同時對于輕質油的生成、運移、保存條件進行了初步分析，認為區塊內有利的烴源巖、有機質生油母質類刑、適當的的圈閉條件，適合的油氣運移充注時間和烴的成熟度，以及埋深等原因是造成區內輕質油富集的主要因素。
  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. By studying the material conditions of entrapment, it is conclude that de nan depression is a low - mature oil kitchen, that main source rock of sha san member is partly mature. 2. the undercompaction starts at the depth of 1300 to 1500 meter

    研究取得的認識如下： 1 、成藏條件研究表明，德南窪陷下第三系生油巖成熟度低，主力生油層在窪陷深部進入生烴門限，德南窪陷是一個低熟油灶。
  9. 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。
  10. This paper concentrates steranes and terpanes in high mature - over mature oil and source rock using distillation method and identifies with column chromatography and chromatography - mass spectrum, achieving better identification effect

    用精餾法對該類原油和生油巖中的甾萜類化合物進行富集，然後通過柱色層分析和色譜質譜鑒定，得到了較為理想的甾萜類化合物鑒定效果。
  11. 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。
  12. The research shows that beir depression characterized as several resources, thin facies, and more kinds of reservoir. the lowstand system tract of nantun formation is the principal target reservoir with best source rock and reservoir. the upper mudstone developed in transgressive system tract of damoguaihe formation is the important regional sealing bed, forming the best oil source bed, reservoir, caprock pattern

    綜合研究表明，貝爾凹陷具有多物源、相帶窄、儲集類型多的特點，南屯組低水位體系域具備生油和儲集條件，是海拉爾盆地的主要勘探目的層段，其上部的大磨拐河組水進體系域發育的泥巖是良好的區域性蓋層，可以構成良好的生儲蓋配置。
  13. Associated with the study of lighter hydrocarbon constituent, carbon isotope, biomarker and inclusions, adopted the technique of oil source correlation on whole oil samples, it can be confirmed that the hydrocarbon source of viscous crude in permian, in the east slope of jimusaer depression, is pingdiquan formation mudstone ; carboniferous oil comes from carboniferous source rock. meanwhile, the causes of oil formation are investigated based on datum of reservior geochemistry : viscous crude of permian is the result of biodegradation and low maturity working together, and that lighter hydrocarbon constituent of carboniferous oil is missing. at last, the mode and mechanism of the oil pool formation are analysed in the study area according to the structure phylogeny, sedimentary history, and data of reservior geochemistry

    本論文根據輕烴、碳同位素、生物標志化合物等資料，運用全烴地球化學油源對比方法進行油源對比，得出吉木薩爾凹陷東斜坡區二疊系的稠油來自平地泉組泥巖，石炭系的稀油來自石炭系本身源巖；同時，根據地化資料研究了原油的成因，認為二疊系稠油是生物降解和成熟度較低共同作用的結果，石炭系的稀油存在輕組分散失現象；最後，綜合構造、沉積、烴源巖和油藏地球化學資料，分析了吉木薩爾凹陷原油的成藏機制和模式。
  14. 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。
  15. The correlation of oil - oil indicated that the oil can be devided into three species at least ; the correlation of oil - source rock indicated that there are three sets of source rock, namely cambrian - ordovician, carboniferous - permian and jurassic system

    油油對比表明原油至少可分為三類；油源對比表明有三套烴源巖，即寒武奧陶系、石炭二疊系和侏羅系生油巖。
  16. 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。
  17. ( 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。
  18. The characteristics of compaction curves, the evolution of organic matter, the direction of migration and assignment, conduit system, fluid potential are studied it is concluded that the low maturity of the source of the eogene age is the main factor to control the entrapment. it controls the direction of the primary migration, confines the location of mature source rock and the special carrier rock, controls the time of expulsion and the amount of petroleum, therefore ; the effective traps should be near to oil kitchen and on the pathways of migration

    認為下第三系油灶的低熟是影響其運聚成藏的關鍵因素，生油巖低熟決定油氣初次排烴的方向指向沙三下段；生油巖低熟決定成熟生油巖分佈的局限性和輸導體的特殊性；生油巖低熟決定起排烴時間晚、生烴量不足，從而決定有效的圈閉應是近源的、在運移主路線上。
  19. 4. it is concluded that the es3 is a main member to accommodate the oil expelled from the source rock of the es3 member, that two assignment units of the type i are prospective areas where faulted reservoirs, fracture reservoirs, lithologic deposits may well be founded. the depth of threshold is among 2600 - 2800 meter and that of expulsion is around 3100 - 3400 meter, so the source rock of sha er member is totally immature and that of sha san member is partly mature

    4 、從歷史演化角度和二次運移理論出發，研究了德南窪陷下第三系低熟油灶的油氣運移作用和分配，提出初次分配主要指向是沙三下段；內部成藏系統是有效的成藏系統，其內部油氣的再次分配主要指向德3井南和德1井南是兩個類油氣分配單元；德南窪陷生烴深度2600 - 2800米間，排烴起始深度在3100 - 3400米間，按目前下第三系地層埋深深度，則沙一段生油巖基本上處于未成熟狀態，沙三中、下生油巖處于低熟狀態，僅在窪陷深部分佈成熟生油巖。
  20. Source rock evaluation and oil - source rock correlation in well yangcan1 of dayangshu basin

    大楊樹盆地楊參1井烴源巖評價及油源對比
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