石炭系 的英文怎麼說

中文拼音 [dàntànxì]
石炭系 英文
carbonic
  • 石 : 石量詞（容量單位, 十斗為一石） dan, a unit of dry measure for grain （= l00 sheng）
  • 炭 : 名詞1. （木炭的通稱） charcoal 2. （像炭的東西） sth. resembling charcoal3. [方言] （煤） coal4. （姓氏） a surname
  • 系 : 系動詞（打結; 扣） tie; fasten; do up; button up
  1. Depositional characteristics of carboniferous in tahe region

    塔河地區石炭系沉積特徵
  2. Reservoir prediction of sand - mud rock of carboniferous in tuoputai

    托浦臺石炭系砂泥巖儲層預測
  3. Intermediate zones of east - slope are in the way of oil travel and favorable territory oil moving to, so they are advantageous potential oil region

    勘探層位以石炭系和二疊系為主。吉木薩爾凹陷斜坡過渡帶也是較為有利的潛在含油區。
  4. According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  5. Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation

    文摘:根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。
  6. The application of prepositive acid fracture technique in the reform of carboniferous oil reservior

    前置液酸壓技術在石炭系油藏改造中的應用
  7. I also define each unite of formation and members. including characters of petrology and regional distribution. finally, the stratigraphical framework have been constructed based on consistencies of petrology, facies and the relationships of rock units

    同時對所劃的各組、段的特徵、含義進行了詳細描述，最後依據巖性巖相特徵、地層接觸關系等，進行了區域對比，建立了該區石炭系的巖石地層格架。
  8. 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。
  9. These deposits, which can be obviously divided into basic and acid volcanic types, are present in the carboniferous bi - model volcanic series and occur along two horizons, i. e., the lower carboniferous mafic volcanic rock and the upper carboniferous felsic volcanic rock

    這些礦床產在石炭系雙峰式火山巖系之內，沿著下石炭統基性火山巖和上石炭統酸性火山巖兩個層位產出，分別以玄武巖和流紋巖為容礦主巖，可以明顯地分成基性火山巖型和酸性火山巖型兩種類型。
  10. Liujiata carboniferous system and related geological aspects in hequ district of shanxi

    山西河曲劉家塔之石炭系及相關地質問題
  11. Gravel features and tectonic implication in the carbonifereous huyoufang formation on the northern margin of dabie orogenic belt

    大別造山帶北緣石炭系胡油坊組礫石特徵及其構造意義
  12. Based on the results of the third hydrocarbon resources evaluation in junggar basin, the amount of the hydrocarbon resources in carboniferous and permian are 1. 35 billion equivalent and 2. 56 billion equivalent respectively, among which the hydrocarbon resources in carboniferous occurs in volcanic rock, while the hydrocarbon resources in permian with one fourth distributed in the volcanic rock of jiamuhe formation

    根據準噶爾盆地第三次油氣資源評價結果，蘊藏在石炭系和二疊系中的油氣資源量約分別為13 . 5億噸（當量）和25 . 6億噸（當量） ，其中石炭系的油氣資源量主要分佈在火山巖中，而二疊系的資源量約有1 / 4分佈在佳木河組的火山巖中。
  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. The geologic condition of carboniferous ~ lower triassic in jianghan plain is of great advantage for hydrocarbon bearing, and these stratum are the important areas for marine hydrocarbon exploration, in spite of more than twenty years " exploration, no commercial discoveries have been achieved yet

    江漢平原石炭系?下三疊統具有優越的成油氣地質條件，是歷年來海相油氣勘探的重點，但經過二十多年的油氣勘探，至今仍未獲得工業油氣流。
  15. One to three karst cycles may be recognized mostly at the top of the upper permian strata, top of the middle permian maokouan strata and top of the carboniferous strata and subordinately at the top of the devonian strata

    這些古巖溶作用主要存在於上二疊統頂部、中二疊統茅口組頂部和石炭系頂部，其次是泥盆系的頂部。
  16. Carboniferous in manxi region of tarim basin is divided into six sequences under the guidance of sequence stratigraphy and in the combination of well logging data and log data, and the characteristics of every sequence and system tract are described

    本文以層序地層學理論為指導，綜合測井、錄井資料，將塔里木盆地滿西地區石炭系劃分為六個層序，並描述了各層序及體系域的特徵。
  17. By use of new theory, views and methods of modern sedimentology and through the analasis of core, well logging and log data of approximately twenty well in manxi area, six kinds of sedimentary facies such as wave - dominated littoral, tide - dominated littoral, mixing littoral, shallow marine r shelf, carbonate platform facies and others are recognized and elaborated

    運用現代沉積學的新理論、新觀點與新方法，通過對滿西地區20餘口井巖芯、錄井和測井資料的分析，識別並闡述區內石炭系浪控濱岸、潮控濱岸、混積濱岸、淺海陸棚和碳酸鹽巖臺地等六種沉積相。
  18. Study of sedimentary facies of bioclastic limestone member, carboniferous, tarim basin

    塔里木盆地石炭系生屑灰巖段沉積相研究
  19. And the author analyses and evaluates hydrocarbon source rock, caprock and trap reserving condition of work area on the base of drilling achievements of 7 emphases structure hi work area. therefore the author draws two conclusion as follow : ( 1 ) the most favorable reservoir of the work area is the spreading region of dolomite rock of carboniferous whose remaining thickness is greater than 20m with the region from jiao 1 well - cizhu 1 well - maan 1 well to west of shizhu county seat. the secondary favorable reservoir of it is the spreading region of dolomite rock with the remaining thickness greater than 10m but less than 20m which is eastern and western region of the most favorable region and the off - lying of yangdu 1 well and yangdu 2 well

    本文研究主要通過地層層序、沉積相、成巖作用和儲集條件等方面對該區石炭系黃龍組碳酸鹽巖儲層進行評價和預測，並且從該區7個重點構造的鉆探成果出發進行烴源巖、蓋層和圈閉保存條件等成藏條件的分析與評價，分別得出以下結論：工區最有利的儲層是石炭系白雲巖殘厚20m的分佈區，位於轎1井?茨竹1井?馬鞍1井?石柱縣城以西地區；較有利的儲層是石炭系白雲巖殘厚10 20m的分佈區，位於級區以東及以西的洋渡1 、 2井外圍；不利的儲層是白雲巖10m及石炭系黃龍組灰巖的分佈區，位於工區西南部和東部地區。
  20. Three angular unconformities found in the field work in the previous baishan formation of the carboniferous in poziquan area help to subdivide baishan formation into four formations

    摘要通過野外工作，在前人所劃的坡子泉地區石炭系白山組內新發現三個角度不整合，而將白山組解體成四個組。
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