organic geochemistry中文是什么意思

• 有机地球化学

• "organic"中文翻译    adj. 1.【医学】器官的；器质性的；有机体的；【化学 ...
• "geochemistry"中文翻译    n. 地球化学。 adj. -ical ,-ist n. ...
• "environmental organic geochemistry" 中文翻译 :    环境有机地球化学
• "marine organic geochemistry" 中文翻译 :    海洋有机地球化学
• "molecular organic geochemistry" 中文翻译 :    分子有机地球化学
• "organic geochemistry method" 中文翻译 :    有机地球化学法
• "geochemistry" 中文翻译 :    n. 地球化学。 adj. -ical ,-ist n.
• "organic" 中文翻译 :    adj. 1.【医学】器官的；器质性的；有机体的；【化学】有机的 (opp. inorganic)。 2.有组织的，有系统的；有机的；结构的；建制的；根本的；生来的，固有的。 an organic disease 器官病。 organic matter 有机物。 organic chemistry 有机化学。 an organic whole 有机统一体。 n. 分子有机体。 adv. -ically
• "agricultural geochemistry" 中文翻译 :    农业地球化学
• "airborne geochemistry" 中文翻译 :    航空地球化学
• "analytic geochemistry" 中文翻译 :    分析地球化学
• "analytical geochemistry" 中文翻译 :    分析地球化学
• "applied geochemistry" 中文翻译 :    应用地球化学
• "aquatic geochemistry" 中文翻译 :    水的地球化学
• "bedrock geochemistry" 中文翻译 :    基岩地球化学
• "biomass geochemistry" 中文翻译 :    生物地球化学; 生物质地球化学
• "comparative geochemistry" 中文翻译 :    比较地球化学
• "core geochemistry" 中文翻译 :    地核地球化学
• "earthquake geochemistry" 中文翻译 :    地震地球化学
• "element geochemistry" 中文翻译 :    元素地球化学
• "environmental geochemistry" 中文翻译 :    环境地球化学
• "exogenic geochemistry" 中文翻译 :    外生地球化学
• "experimental geochemistry" 中文翻译 :    实验地球化学
• "exploration geochemistry" 中文翻译 :    勘查地球化学; 勘探地球化学
• "gas geochemistry" 中文翻译 :    气体地球化学; 天然气地球化学

• Application of organic geochemistry in study of hydrocarbon source and maturity
  核磁共振技术在石油地球化学研究中的应用
• Organic geochemistry of penguin ornithogenic sediment from ardley island , west antarctica
  南极阿德雷岛企鹅粪土沉积物分子地球化学特征
• Geological feature of kenxi area is described from the analysis of evolution history of structure , accumulation , organic geochemistry and dynamic system of reservoir
  从综合分析垦西地区构造演化史、沉积演化史、有机地化及成藏动力学系统出发，对垦西地区的地质特征进行了描述。
• Based on the study of organic geochemistry and organic lithology , this paper mainly discussed the question of the hydrocarbon generating potential and contribution of hydrogen - rich maceral in liupanshui area , guizhou province
  从有机岩石学与有机地球化学角度研究烃源岩有机质成烃演化和生烃作用是油气资源评价的一个重要方面。
• Abstract : based on the study of organic geochemistry and organic lithology , this paper mainly discussed the question of the hydrocarbon generating potential and contribution of hydrogen - rich maceral in liupanshui area , guizhou province
  文摘:从有机岩石学与有机地球化学角度研究烃源岩有机质成烃演化和生烃作用是油气资源评价的一个重要方面。
• The author studied meticulously the nongba sections , abundant data was achieved . besides the basic sreatigraphy study , on the aspects of paleontolgoy , organic geochemistry and thrust slice type stratigraphy , et al . ,
  本文除了对剖面进行基础性的地层学研究之外，从古生物学、有机地球化学、造山带区域地层学和古地理等多方面开展卓有成效的工作。
• 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。
• There have been many questions about the petroleum pool formation conditions and models for this area since the first well was drilled in 1988 , which has had an great influence on the further petroleum exploration and development . in this study , a method with the combination of petroleum geology , sequence stratigrapy , organic geochemistry and geophysics , based on drilled core analysis data , well data and seismic sections , has been applied to investigate the petroleum pool formation conditions and models in this area , and the following results and recognition have been obtained : ( 1 ) . the lower tertiary strata are subdivided into two sequences and seven systems
  本研究以钻井取心分析资料、测井数据、地震资料为基础，综合利用沉积学、层序地层学、石油地质学、地球物理学、有机地球化学等多门学科的有关理论和研究方法，通过对埕岛东斜坡区油气藏形成条件和模式研究，主要取得了以下几个方面成果和认识： ( 1 )埕岛东斜坡地区下第三系共划分两个层序、七个体系域，其中沙一段至东三段中下部沉积为层序，东三段上部至东一段为层序。
• The essential elements and process of gas reservoir formation of ordovician in ordos basin have been annalysed systematicly and scientificly by means of the theory and method of organic geochemistry and tectonic geology in this dissertation . the several advanced techniques , such as gas generation thermal simulation , on - line individual gas compounds carbon isotope determination ( py - gc - c - ir - ms ) , the analysis technique of light hydrocarbons and biomarkers in natural gas , gas migration simulation and gas carbon isotope determination in fluid inclusions , have been applied to focuse on the study of the gas generation mechanism of souce rock , correlation between gas and source rock , reservoir formation history , migration direction , charging road in detail
  应用有机地球化学和构造地质学理论和方法对鄂尔多斯盆地奥陶系天然气地质研究中薄弱环节成藏要素和作用进行了系统科学分析。利用烃源岩生气定量热模拟技术、热模拟在线碳同位素实验技术、气体轻烃和生物标志物分析技术、运聚成藏物理模拟技术和包裹体中碳同位素分析技术等多种先进的实验技术对烃源岩的生气机理、气源和混合比、成藏史、充注路径、运移方向和构造作用与成藏关系等问题进行了深入的研究，在前人研究的基础上，经过本次大量的实验分析和综合研究，提出了一些新的认识。
• Phosphate deposits are distributed along the margin , platform and basin in the west yangtze area . the analysis methods include the paleogeography , petrology , organic geochemistry , geochemistry . the conclusions are drawn that the source of phosphate deposits distributed along the margin originate from the weathering production of continent , while phosphate deposits along the platform and basin gain phosphorus through hot spring on the buttom of the sea floor , which is brought to the sedimentary environment by rising sea - fluid , then accumulated by the organism and microorganism , meanwhile , basin phosphorite keep relatively higher organic carbon content
  认为早寒武世早期古陆遭受风化，被剥蚀下来的产物成为潮坪型磷块岩的主要磷质来源，在碳酸盐岩台地发生的热点活动和上升洋流从盆底深部带来的磷质，共同作为台地型磷块岩的磷源，盆地型磷块岩的磷质同样是由热点活动和上升流携带至缺氧的沉积环境中，通过藻类或微生物的富集作用成岩，并保留了较高的有机碳含量。

• organic geochemistry 意味
• organic geochemistryとは意味有機地球化学｛ゆうき ちきゅう かがく｝