油巖 的英文怎麼說

中文拼音 [yóuyán]
油巖 英文
kerogen
  • : Ⅰ名詞1 (脂肪; 油脂) oil; fat; grease 2 (姓氏) a surname Ⅱ動詞1 (用桐油、油漆等塗抹) apply t...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. 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,主力生層在窪陷深部進入生烴門限,德南窪陷是一個低熟灶。
  2. Identification of source rocks by quick methods, and quantitative evaluation of their petroleum potential can be done either in the laboratory or on the well-site.

    無論在實驗室或井場都能用快速方法鑒別生油巖並對其生能力作出定量估價。
  3. Active source rock

    有效生油巖
  4. The course mainly introduce the profession standard of petroleum, which including the standard of petroleum geology survey and exploration work, the technical standard of basin research, the detailed rules of trap description, the standard of reservoir description, the technical standard of seismic data interpretation, the technical standard of test well geological work, the standard of oil - bearing rock system ' s classification and correlation, the standard of oil and gas reserves, the criterion of reservoir evaluation, the schedule standard of exploration project design and so on

    本課主要介紹石天然氣行業標準,包括石天然氣地質調查與勘探工作規范、盆地研究技術規范、圈閉描述工作細則、藏描述規范、地震資料解釋技術規范、探井地質工作技術規范、含油巖系劃分與對比規范、石與天然氣儲量規范、儲層評價標準以及勘探項目設計編制規范等內容。
  5. 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。
  6. Abstract : yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    文摘:陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲田,儲集層主要為三角洲砂體,壓實作用和膠結作用強烈,儲層非均質性非常嚴重,因此預測次生孔隙發育帶是尋找氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外,還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致,從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中,並沿著有利儲集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異常壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  7. Yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲田,儲集層主要為三角洲砂體,壓實作用和膠結作用強烈,儲層非均質性非常嚴重,因此預測次生孔隙發育帶是尋找氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外,還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致,從而在異常壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中,並沿著有利儲集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異常壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  8. The ordos basin is an important terrestrial basin that came into being during mesozoic in our country. the yanchang formation more than one kilometer in thickness is the main oil - bearing beds in the study area. its lithology characteristic indicated that the formation was deposited in fluvial - lacustrine environment

    鄂爾多斯盆地是我國十分重要的中生代內陸盆地,厚逾千米的上三疊統延長組是區內主要的含油巖系,其性特徵表現為河流-湖泊相的陸相沉積。
  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段。
  10. 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

    對比表明原至少可分為三類;源對比表明有三套烴源,即寒武奧陶系、石炭二疊系和侏羅系生油巖
  11. 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

    認為下第三系灶的低熟是影響其運聚成藏的關鍵因素,生油巖低熟決定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。
  12. 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灶的氣運移作用和分配,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,其內部氣的再次分配主要指向德3井南和德1井南是兩個類氣分配單元;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
  13. East china sea shelf basin, consisting of tertiary oil - bearing strata and great in thickness, is an important cenozioc oil - bearing basin in china

    摘要東海陸架盆地是我國重要的新生代海上含氣盆地,其中充填了巨厚的古新近系含油巖系。
  14. Standard guide for use of rotary kiln produced expanded shale, clay or slate as a mineral amendment in topsoil used for landscaping and related purposes

    園林設計及其有關用途的作為上層土中改良礦物質用旋轉窯生產的空心油巖粘土或石片的使用標準指南
  15. Oil - source correlation analysis has shown that the oils were mostly from ed2 source rocks from the bozhong depression, and the oils occurred in the slope hidden hill belt were from es3 or / and es, source rocks in the bozhong depression

    源對比結果表明東斜坡帶東營組原來源於渤中凹陷ed _ 2暗色泥,斜坡潛山帶原來源於渤中凹陷es _ 3或es _ 1生油巖
  16. The hydrocarbon groups, alkane hydrocarbons and biological markers in the crude oils and the oil source rocks have closed relationships, which has shown that zifusi lw - lying area has a better oil source condition and oil source potentiality

    在原和生油巖中烴類族組分、烷烴和生物標志物之間均有較好的親緣關系,表明資福寺窪陷具有較好的生條件和生潛力。
  17. Steranes and terpanes in high mature - over mature oil and source rock cannot be identified well because of their quite low content

    對于高成熟過成熟的原和生油巖,由於甾萜類化合物含量大低往往鑒定效果不好或根本檢測不到。
  18. Steranes and terpanes exist in saturated hydrocarbon component of oil and source rock, and they are usually identified by gas chromatogram - mass spectrum

    甾萜類化合物存在於原和生油巖的飽和烴組分中,通常用色譜質譜法鑒定。
  19. It was noted that the upper mesozoic strata ( mainly cretaceous ) as revealed by drill or dredge from the eastern nansha waters might extend into the hinterland of the nansha waters

    南海裂谷期間形成的下第三系具有明顯的裂谷充填特徵,其構成生油巖主體。
  20. Studies on the combination of source rocks and reservoirs show that yuejin - dongchaishan, dafengshan and the front part of arjinshan area are the most favourable areas for oil and gas accumulation

    根據生油巖及儲油巖疊置組合關系,指出阿爾金山前地區、躍進東柴山地區、大風山地區是有利氣聚集區。
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