稀熟油 的英文怎麼說

中文拼音 [shúyóu]
稀熟油 英文
thin stand oil
  • : Ⅰ形容詞1 (事物出現得少) rare; scarce; uncommon 2 (事物之間距離遠; 空隙大) sparse; scattered 3...
  • : 熟形容詞1 (植物的果實完全長成) ripe 2 (加熱到可以吃的程度) cooked; done 3 (加工製造或鍛煉過...
  • : 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...
  1. 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,運用全烴地球化學源對比方法進行源對比,得出吉木薩爾凹陷東斜坡區二疊系的稠來自平地泉組泥巖,石炭系的來自石炭系本身源巖;同時,根據地化資料研究了原的成因,認為二疊系稠是生物降解和成度較低共同作用的結果,石炭系的存在輕組分散失現象;最後,綜合構造、沉積、烴源巖和藏地球化學資料,分析了吉木薩爾凹陷原的成藏機制和模式。
  2. This oil is derived from the deep buried, mature source rocks of tenggeer formation and aershan formation ii

    屬于成度較高的源來自深部騰格爾組和阿二段成烴源巖。
  3. Cream holding vat

  4. The biomarker characteristics of these two types of viscous oils are distinctive. oil source correlation results show the altered viscous oils were generated from the es3 source rocks and subsequently suffered biodegradation, oxidation and water washing effects near the surface. there exists huge thick alluvial glutinite in luojia - kenxi area, with various physical properties

    兩類稠生物標志物組成也有明顯的差異,次生稠主要由來源於沙三段源巖的正常原)經生物降解、地表氧化、水洗等次生作用形成的,並且成度指標相對較高。
  5. It appears that biodegradation, oxidation and water washing near the surface are not responsible for the high density and high viscosity of these deep viscous heavy oils, in addition, biomarker parameters demonstrate maturities of these viscous oils are relatively low to that of the normal oils derived from the es3 source rocks in this area

    這表明這兩個地區深層稠屬原生稠,不是由於生物降解、地表氧化、水洗等次生作用形成的。生物標志物成度指標顯示稠具有中低成度,相對低於來源於沙三段源巖度。
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