烴源巖類型 的英文怎麼說

中文拼音 [tīngyuányánlèixíng]
烴源巖類型 英文
type of hydrocarbon source rock
  • 烴 : 名詞[化學] （碳氫化合物） hydrocarbon
  • 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
  • 類 : Ⅰ名1 （許多相似或相同的事物的綜合; 種類） class; category; kind; type 2 （姓氏） a surname Ⅱ動詞...
  • 類型 : type; mold; form; cut類型論 theory of types; 類型語句 [計算機] type statements
  1. Through studying it is shown that in chagan sag, the geothermal gradients in the center are higher than those around the sag margin and major factors influencing the characteristics of temperature field distribution are the property of geotectogenesis and the differences in tectonic portion, lithology and underground water behaviour ; there are three types of mudstone compaction, i. e. normal compaction, undercompacition and overcomepaction ; there are two pressure systems in sandstone reservoirs, i. e. normal pressure and negative pressure systems and the strata ' s being uplifted and denuded is the key factor leading to the formation of the negative pressure system in reservoir ; and the distinctive temperature - pressure field characteristics in the sag are possessed of important petroleum geological significance in hydrocarbon source maturity, hydrocarbon generation, widening on oil and gas exploration domain and selecting exploration targets, etc

    研究表明，查干凹陷中心的地溫梯度高於凹陷邊緣，大地構造性質及所處構造部位、巖性與地下水活動的差異是影響凹陷地溫場分佈特徵的主要因素；泥巖壓實存在正常壓實、欠壓實和過壓實三種類型，砂巖儲層段壓力類型可分為正常和負壓兩個系統，地層抬升剝蝕是導致儲層負壓系統形成的主導因素；凹陷獨特的溫壓場特徵對烴源巖成熟、油氣生成、油氣勘探領域的擴大及勘探方向的選擇等具有重要的油氣地質意義。
  2. Dongpu sag is of the superior geological conditions for forming deep gas pools, including two sets f premium source rocks, variety of sand bodies, sell developed porosity and thick halite and mudstone as cap rocks

    摘要東濮凹陷具有形成深層氣的優越基礎地質條件：兩套優質烴源巖、多種類型的儲集砂體和高異常孔隙發育、厚的巖鹽和泥巖作為良好蓋層。
  3. The main strata in this depression are of cretaceous. according to the organic carbon content, kerogen type and maturity, three source rocks have been identified : duhongmu i, tenggeer formation and aershan ii

    根據烴源巖有機質含量、類型和成熟度確認白音查于凹陷有三套烴源巖：都紅木組一段、騰格爾組和阿爾善組二段。
  4. 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。
  5. On the basis of analyzing and chemically examining a large numble of samples, through comprehensively studying the reservoiring geological conditions as hydrocarbon generation, petrophysical property, reservoir - caprock assemblage and lithologic trap type, by use of mathematical statistics, it was considered that yulin gas field is located in the greatest hydrocarbon - generating intensity area in the basin and its hydrocarbon source rocks are the permo - carboniferous coal measure strata, thus possessing the material conditions of forming large - sized gas fields

    通過大量的化驗分析樣品數據，採用數理統計的方法對生烴條件、儲層物性、儲蓋組合配置、巖性圈閉類型等成藏地質條件進行了較為深入的研究，認為榆林氣田處于鄂爾多斯盆地最大生烴強度區，其烴源巖為石炭二疊系煤系地層，具備形成大型氣田的物質條件。
  6. The regularity of accumulation distribution is ascertained and directs the exploration orientation. the main results obtained in this paper are : 1. the analyses of hydrocarbon - bearing rock, reservoir, caprock and oil & gas reservoir indicate the source of oil & gas, the space for reservoir, requirement for preservation, reservoir type and its basic characters. 2. it is realized by the analyses of sealing up capability of caprock and faults, and fault ' slatter stability from microcosmic and macroscopic that the wide - spread regional caprock of nm t prevented oil & gas of neogene from diffusing fault movement in neogene less violated and fault displacement decreased, which are advantageous for the preservation of oil & gas reservoir. and latter structure movement usually formed the accunulation of oil & gas in neogene. 3. the research of history of hydrocarbon generation and expulsion of main hydrocarbon - bearing rock in qikou depression reveals the threshold depth and the fime of hydrocarbon generation and expulsion

    項目研究取得了如下認識： 1 、對烴源巖、儲集層、蓋層及油氣藏展開分析，明確了歧口凹陷上第三系油氣藏的油氣來源、儲集場所、保存條件和油氣藏類型及其基本特徵； 2 、從微觀和宏觀上對蓋層的封蓋能力以及斷層封堵和後期穩定性進行分析，認識到明下段區域蓋層的廣泛分佈阻止了上第三系油氣藏的油氣逸散，同時上第三系斷層活動減弱，斷距較小，對油氣藏的保存較為有利。
  7. 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。
  8. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據沉積相帶與沉積環境的不同，可將烴源巖劃分為在不同沉積環境中的4種類型烴源巖；臺地邊緣灰泥丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海盆地型烴源巖。
  9. 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。
  10. By analyzing reserve forming conditions of high evolution marine strata, including types of hydrocarbon source, the structural evolution, the condition of preservation and so on, it is considered that under the background of intensive structural movements, the " second " compensatory capabilities of the hydrocarbon source in the middle and lower yangtze region and regional preservation conditions would be the major factors to control the enriched oil and gas collection in this region

    從分析高演化海相地層的烴源類型、構造演化以及整體封存等成藏條件，認為中、下揚子地區在強烈的構造運動背景下，烴源巖的「再次」補給能力和區域保存條件將成為控制中、下揚子地區油氣富集的主要因素。
  11. 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。
  12. 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。
  13. This type of oil is derived from the shallowly buried, immature or lowly mature source rock of duhongmu formation i. the type 1 and 2 oils are two basic types in daerqi oilfield

    這類原油屬于原生低成熟特稠油，油源為都一段未熟、低成熟烴源巖。第一和第二類原油為達爾其油田基本的原油類型。
  14. After field profiles being observed and some indoor tests and analysis being fulfilled, this paper researched distribution, organic type and abundance of the xujiahe formation, upper triassic in chishui and other areas in the sichuan basin, analysed the main geo - chemical characteristics of the gas from the xujiahe formation, discovered the source characteristics of the xujiahe formation, and discussed the origin of the natural gas found in the formation

    摘要細致觀測了野外剖面，並進行了相關的室內分析化驗，對比研究了赤水地區與四川盆地其他地區上三疊統須家河組烴源巖分佈特徵、有機質類型及豐度，結合赤水地區須家河組天然氣的主要地球化學特徵，揭示了赤水地區須家河組的源巖特徵，初步探討了其天然氣成因。
  15. The maturity degree of source rocks is high, but quality diversity exists within different source rocks

    結果表明，烴源巖中含有豐富的有機質，其類型以型乾酪根為主，部分為型乾酪根。
  16. Based on the maturity, organic matter richness, organic type of source rocks, following order have been proposed based on quality of source rocks : 2 ) the curve between tmax and depth has been established. from the data of different wells, it indicates that most of the source rocks in this region belong to immature source rocks. the data also reflect the early generation of hydrocarbon in the source rocks

    取得的主要成果如下： 1 、通過綜合分析德南窪陷烴源巖品質、生烴潛量、有機質類型和豐度，得出研究區沙一段和沙三段為好-較好烴源巖，有機質以-型有機質為主，生烴潛力較強；沙四段烴源巖為較差-較好烴源巖，有機質類型變化較大；沙二段有機質類型差，生烴潛力十分有限，為非烴源巖。
  17. 5. with the help of thermal history of hydrocarbon source rock, and combined with the types, physical characters and homogeneous temperature distribution of organic and salty solution fluid inclusion with different types in ordovician limestones, the formation time and migration stages of oil and gas are determined

    5根據烴源巖熱演化史，結合奧陶系灰巖中不同類型的有機和鹽水溶液包裹體類型、物理特徵和均一溫度分佈，確定了油氣的形成時期和運移期次。
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