标志化合物的英文

• labelled compound

• "标志"英文翻译    sign; mark; symbol; hallmark ...
• "化合物"英文翻译    chemical compound; compound
• "生物标志化合物" 英文翻译 :    biomarker
• "同位素标志化合物" 英文翻译 :    isotopically labeled compound
• "标志化石" 英文翻译 :    guide fossil
• "标志化舞蹈" 英文翻译 :    danse caracterises
• "化合物" 英文翻译 :    chemical compound; compound 高分子化合物 high polymer; highly polymerized compound
• "化合物a" 英文翻译 :    compd a
• "化合物s" 英文翻译 :    compd s; compound s; desoxycor tisone
• "化合物,复合物" 英文翻译 :    compound
• "标志化石（曾用名“标准化石”）" 英文翻译 :    index fossil
• "环化合物, 闭链化合物" 英文翻译 :    cyclic compound
• "母化合物；亲体化合物" 英文翻译 :    parent compound
• "化合物混合物" 英文翻译 :    compound
• "氨化合物" 英文翻译 :    ammonium compound
• "氨基化合物" 英文翻译 :    amide; amino compound; amino-compound
• "氨类化合物" 英文翻译 :    ammoniacal compounds
• "安定化合物" 英文翻译 :    stable compound
• "胺类化合物" 英文翻译 :    amine-group compound
• "八环化合物" 英文翻译 :    cctocyclic compound
• "半水化合物" 英文翻译 :    hemihydrate
• "包藏（容）化合物" 英文翻译 :    inclusion compound
• "包含化合物" 英文翻译 :    clathrate compound; inclusion compound
• "包合化合物" 英文翻译 :    inclusion compound
• "饱和化合物" 英文翻译 :    satisfied compound; saturate compound; saturated compounds

• Biomarker compounds of kujieertai uranium deposits
  库捷尔太铀矿床的生物标志化合物研究
• Steranes and terpanes are widely used in petroleum geochemistry study since they are important indexes for oil sources correlation and oil and gas migration
  摘要甾萜类生物标志化合物作为油源对比和油气运移的重要指标，在油气地球化学研究中得到了广泛的应用。
• Biomarker has a wide application in the research of petroleum geology , such as different types of organics thermal evolution , ancient sediments ' environment and so on
  摘要生物标志化合物在石油地质中应用广泛，可应用于源岩有机质类型和古沉积环境评价以及热演化阶段的确定等。
• In this paper , the stereoisomer rearrangement of biomarker compound for the exclusive reaction form the electronic off - domain to the out - proton magnetic rotation is interpreted in the sedimentary system in terms of the micro - particle wave motion and the molecular orbital theory
  摘要应用微观粒子波动和分子轨道理论、解释生物标志化合物在沉积体系中自身独有的“电子离城外质子磁旋反应”的重排机理。
• The geochemical characteristics of coals from liyazhuang coal mine , sihe coal mine and fucheng coal mine of qinshui basin , shanxi province , were comparatively studied , and the thermal evolution degree , the contents of soluble organic matter and the biomarker characteristics of coals were discussed
  摘要对比研究了山西沁水盆地李雅庄煤矿、寺河煤矿和附城七一煤矿煤岩的地球化学特徵，讨论了煤岩的热演化程度、可溶有机质含量、生物标志化合物特徵。
• 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
  本项研究以德南洼陷重点烃源岩- - -下第三系沙河街组为对象，应用有机地球化学理论与方法对其有机质类型和丰度、成熟度、生烃潜量等进行研究；通过特征生物标志化合物的分析，阐明研究区未熟-低熟烃源岩母质构成、沉积环境和成熟演化；通过油源对比和生烃条件综合分析，提出本区烃源岩生烃机制，建立未熟-低熟烃源岩有机质生烃模式。
• The paper adopts some methods such as gas composition , carbon isotope , systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas , illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian , comes from carbonatite hydrocarbon rocks permian which most of them are overmature , its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves , presents in geochemistry characteristics of oil type cracked gas
  摘要通过对川中川南过渡带西部的磨溪潼南地区嘉二段天然气组成、碳同位素组成、高演化天然气储层沥青生物标志化合物的系统分析测试和混合成因气的定量估算，阐明了该区嘉二段天然气主要属于二叠系腐泥型有机质成因气，来源于二叠系过成熟为主的碳酸盐岩烃源，主力气源与嘉陵江组自身的碳酸盐岩烃源无关，并具有油型裂解气的地球化学特征。
• We can see that es3 and es4 source rocks contributes greatly to the formation of immature oil . other oil source correlation also show that the immature oil originated from source rocks of es3 and es4 in this region . 7 ) the existence of high abundance of sulfid in the mudstone indicate that that there is a relatively high salinity environment in source rocks which is favorable for algae growth
  4 、通过稳定碳同位素、甾烷和萜烷等不同的生物标志化合物参数分析探讨了研究区德1井低熟油的物源，生物标志化合物图谱指纹对比表明，德1井沙一段( es _ 1 )油来源于本段烃源岩，德1井沙四段( es _ 4 )原油主要来源于沙四段泥岩和沙三段中、下部泥岩，为自生自储成因。
• First of all , the theoretic basis for the stereoisomer rearrangement of biomarker compound is illustrated , and then the corresponding relations between the sterane / terpane stereoisomer rearrangement and maturity , as well as the polarity / non - polarity and petroleum migration are discussed , respectively
  首先阐明生物标志化合物立体异构重排的理论依据：然后分别探讨了萜、甾烷类立体异构重排和成熟度对应关系；极性、非极性生物标志化合物异构体重排和油气运移对应关系。
• 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
  本论文根据轻烃、碳同位素、生物标志化合物等资料，运用全烃地球化学油源对比方法进行油源对比，得出吉木萨尔凹陷东斜坡区二叠系的稠油来自平地泉组泥岩，石炭系的稀油来自石炭系本身源岩；同时，根据地化资料研究了原油的成因，认为二叠系稠油是生物降解和成熟度较低共同作用的结果，石炭系的稀油存在轻组分散失现象；最后，综合构造、沉积、烃源岩和油藏地球化学资料，分析了吉木萨尔凹陷原油的成藏机制和模式。