海相富有机碳沉积,marine organic carbon-rich sediments
1)marine organic carbon-rich sediments海相富有机碳沉积
1.Based on the previous discussion about geological setting and major controlling factors on the marine organic carbon-rich accumulation,this paper proposes that both high primary productivity(PP) and oceanic anoxic events(OAE) controlled the wide distribution ofmarine organic carbon-rich sediments in the mid-Cretaceous.白垩纪中期(约125～88Ma)海相富有机碳沉积广泛发育于全球各主要洋盆和沉降区,是许多大油田的重要烃源岩。
英文短句/例句
1.Geobiological setting of the marine organic carbon-rich accumulation in mid-Cretaceous白垩纪中期海相富有机碳沉积的地球生物学背景
2.A simple analysis of influential factors for Cretaceous marine organic-rich sediments in Southern Tibet藏南地区海相白垩系富有机质沉积的影响因素浅析
3.Biogeochemical Characteristics of Organic Carbon in Surface Sediments From the Chukchi Sea北极楚科奇海海底表层沉积物有机碳的生物地球化学特征
4.The Reaction of Bacteria in the Deep Sea Sediment to Organic Carbon: Effects on Bac terial Community and Enzyme Activity;深海沉积物中细菌对有机碳源的反应：细菌群落和酶活的变化
anic Carbon Distribution in the Yangtze River Estuary-Hangzhou Bay and Its Adjacent Sea Area长江口—杭州湾及其邻近海域不同粒级沉积有机碳分布特征
6.Characteristics of Organic Matter in the Sediment of wuliangsuhai lake and its Relationship to the Eutrophication乌梁素海沉积物有机质特征及其与富营养化的关系
7.EOGENE LACUSTRINE CARBONATE ROCKS AND SEDIMENTARY MODEL IN BOHAI BAY REGION渤海湾地区下第三系湖相碳酸盐岩及沉积模式
8.The Forms of Organic Phosphorus、Organic Carbon of Lake Sediment and Their Translation and Transplant;湖泊沉积物有机磷、有机碳形态及其迁移、转化
9.Research of Sedimentary Facies and the Distribution of Sand Body of the Triassic Yangchang Formation in Fuxian Exploration Area of the Ordos Basin;富县探区三叠系延长组沉积相及有利砂体展布
10.Sorption Behavior of Phenanthrene to Natural Carbonaceous Sediments天然富碳沉积物中菲的吸附行为研究
11.sludge (rich in organic matter) that accumulates at the bottom of lakes or oceans.堆积在湖底或海底的软泥（富含有机物）。
12.A Primary Research on the Distribution and Vertical Flux of POC and PN in East China Sea;黄东海颗粒有机碳、氮的分布及沉降通量估算
13.Spatial and Temporal Variations of Sedimentary Organic Matter Origin and Accumulation Rate in the Pearl River Estuary and Adjacent Coastal Waters of South China Sea珠江口和邻近海域沉积有机质的来源及其沉积通量的时空变化
14.A preliminary study of oxygen and carbon isotopic changes of planktonic foraminifera from surface sediments and plankton tow samples in southern South China Sea南海南部水体和沉积物中的浮游有孔虫氧碳同位素分析
15.A BASIC MODEL OF THE ANCIENT MARINE ENVIRONMENT FOR SEDIMENTATION OF CARBONATE论古代海洋碳酸盐沉积环境基本模式
16.Pyrolysis Mechanism of Carbon Matrix Precursor Cyclohexane for the Rapid Densification Process;快速液相沉积致密化工艺碳前驱体环己烷的热裂解机理
17.Mechanism and Influencing Factors on Surface Roughness of Ultra-smooth Polishing of Chemical Vapor Deposition Silicon Carbide化学气相沉积碳化硅超光滑抛光机理与表面粗糙度影响因素
18.They do not have an illuvial horizon enriched with either silicate clay or with an amorphous mixture of aluminum and organic carbon.没有富含硅酸盐粘土或铝－有机碳非晶质混合物的淀积层。
相关短句/例句
euxinic deposition富有机质沉积
3)organic facies沉积有机相
1.The Jurassic hydrocarbon source rocks on the north margin of Qaidam Basin could be divided into highstand marsh peatorganic facies, forest marsh peat organic fades, shore-shallow lakeorganic facies and semideep-deep lakeorganic facies.根据柴达木盆地北缘侏罗系烃源岩的有机岩石学、沉积学和有机地球化学特征将烃源岩的沉积有机相划分为４种类型，即高位泥炭沼泽有机相、森林泥炭沼泽有机相、滨浅湖有机相和半深湖－较深湖有机相。
2.Directed by the theories such as Petroleum geology and Petroleum geochemistry,the source rocks of late cretaceous in Changling sag of southern Songliao basin are divided intoorganic facies A,organic facies B andorganic facies B-C on the basis of the characteristics of organic petrology,sedimentology and organic geochemistry.以石油地质学和石油地球化学为理论指导,通过对长岭凹陷上白垩统烃源岩的有机岩石学、沉积学和有机地球化学特征的综合分析,将沉积有机相划为3种类型,即有机相A、有机相B和有机相B-C。
4)sedimentary organic facies沉积有机相
1.According to the organic petrology,sedimentology and organic geochemistry of source rocks,thesedimentary organic facies in this area can be divided into three types:hemideep-deep lacustrine organic,shore-swamp organic and high-stand swamp organic facies.根据其有机岩石学、沉积学和有机地球化学的特征,将该区沉积有机相划分为3种类型:高位沼泽有机相、滨浅湖-沼泽有机相和半深湖-深湖有机相。
2.According to the characteristics of organic petrology, sedimentology and organic geochemistry, the source rocks of the Yanchang Formation in Zhenyuan - Jingchuan area in the south of Erdos basin are divided into threesedimentary organic facies including delta, coastal - shallow lake and semi - deep lake.根据鄂尔多斯盆地南部镇原—泾川地区延长组烃源岩的有机岩石学、沉积学及有机地球化学特征将其划分为三种沉积有机相类型:三角洲有机相、滨浅湖有机相以及半深湖—较深湖有机相。
3.Being synthetically analyzed with methods of organic geochemistry, organic and/or sedimentary petrology, the Xishanyao formation is divided into foursedimentary organic facies, which are high moor, forest swamp, running water swamp, and open water organic facies, with the running water swamp and forest swamp being the main facies of hydrocarbon forming.以准噶尔盆地中侏罗统西山窑组为研究对象，通过有机岩石学、有机地球化学和沉积学的综合研究和分析，将西山窑组沉积期划分为四种沉积有机相：高位沼泽有机相，森林沼泽有机相，流水沼泽有机相和开阔水体。
5)organic vapor phase deposition有机气相沉积
6)sedimentary matter湖相沉积有机质
延伸阅读
金属有机化合物化学气相沉积分子式：CAS号：性质：用金属有机化合物热分解进行气相外延生长的方法。其基本原理是将含有外延材料组分的金属有机化合物气体通过载气输送到反应室，在一定温度下进行外延生长。MOCVD技术主要应用于III-V族II-VI族化合物半导体超晶格量子阱等低维材料生长和多元固溶体的多层异质结构材料的生长，还可用于制备高温超导薄膜，铁电薄膜，传感器薄膜，太阳能电池薄膜及其他金属薄膜。该技术工艺可控，操作简便及适用于大规模生产等优点。其缺点是所用源材料为易燃剧毒物质。
