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With the rich sediments supplied by the Pearl River, under the paleogeography sedimentary background of Baiyun Sag continuously subsiding, with sedimentary sequences related to relative transgressive sea level change ,contrary to regressive eustasy, the Pearl River Deepwater Fan System has specific evolution characteristics, which left the sedimentary record controlled by peripherical significant geological events.

珠江深水扇系统以珠江为沉积物源、以持续深沉降的白云凹陷为沉积古地理背景、以与全球海退型海平面相反的相对海侵型海平面变化的沉积层序构成了其发育演化的特殊性,并留下了控制沉积的周边重要事件的记录。23.8 Ma等界面沉积速率和岩石地球化学特征均有突变,反映出物源区的变化,可能折射出与青藏高原隆升、南海扩张有关的重要事件,使得古珠江骤然向西部高原拓展,甚至较今天的珠江流域范围还广阔;承载珠江深水扇系统的白云凹陷持续沉降形成了陆坡内盆地,导致21~10.5 Ma BP多个层序深水扇垂向叠置充填的特殊沉积建造;根据60多口井资料建立的相对海平面变化曲线,具有与全球海平面变化相一致的三级旋回和不一致的二级旋回。

In the basis of the facies markers and facies analysis of principle, there are mainly river、delta and lake depositional sysytems in Upper Triassic of Nanniwan field,in which all kinds of difference sedimentary subfacies and sedimentary microfacies are distinguished, such as meandering river、delta plain、delta front、submerged distributary river course、frontal sheet sand and so on.

利用收集到的各种相标志和相分析原则,对研究区的沉积相进行了比较细致的研究,将南泥湾探区上三叠统分为河流、三角洲、湖泊三种沉积体系,并在各沉积体系中细划出曲流河、三角洲平原、三角洲前缘、浅湖等沉积亚相和水下分流河道、河口坝、前缘席状砂等沉积微相。

The gravity current deposition also may, according to different environment, includes the fan like deposition system (submarine fan or sublacustrine fan), the channel or the trough valley deposition system, bedded or banded deposition system and so on.

重力流沉积还可以按其发育的沉积环境而划分为扇状沉积体系、沟道或槽谷沉积体系、层状或带状沉积体系等。

Type-B Nodule: The source of elements in the nodules comes from slow deposition of the overlying water and the diffusion of the pore water, which comes mainly from the double decomposition reaction of Fe, Mn oxides caused by the oxidation diagenesis of organic material in sediment and its forming process and distribution is controlled by pH in the pore water. There is no corrlation between distribution of the nodules and water depth, topograph.

A型结核主要分布于深海火山沉积环境区,受上覆水Mn〓和Eh制约;B型结核一方面由于在深海火山沉积环境区,受生物作用影响,另一方面在生物沉积环境区,又受火山作用影响,使此类结核的分布与大洋地貌和沉积物的关系不明显;C型结核主要分布在太平洋CCD范围内,受沉积环境上生物和活性有机碳的制约。

According to the analysis of features of the key outcrop sequence stratigraphy, build the sequence frame, through the section comparison, and the study of feature of the 5 key outcrops, then it can be concluded that, conglomerate on the denudation plane or the other contrastive sediment are the main features surrounding the bottom border of the sequence. In the foreland basin sediment environment, the transilient group of mud rock and sandstone are the main sediment features of low-stand system tract. Thick mud rock and sandstone interbedded is the chief component of transgressive system tract, sometimes together with thick turbidity current sandstone; High-stand system tract is composed by the combination of mud rock and sandstone interbedded, with the progradation as its main style. Maximum flooding surface Sediment are usually mudstone, and the thickness is different from each other.

依据关键露头剖面高精度层序特征分析,通过剖面对比建立高精度等时层序地层格架,通过对5条关键露头剖面的详细高精度层序特征分析,认识到:剥蚀面上的粗碎屑岩或与之可区域对比的其它沉积是层序底部边界附近的主要沉积特征;在盆地沉积环境中,砂泥岩发育,厚层、块状砂岩与泥质岩类的突变组合是低位体系域的主要沉积特征;湖进体系域以厚层泥岩夹砂岩为主,有时夹厚度较大的重力流砂体;高位体系域为砂泥互层沉积组合,以进积式叠加样式为主;最大湖泛面多为泥岩,但其厚薄不一。

Results The damp fans, rivers and lakes are main sedimentary systems in Yanqi Basin. They are funned from T(subscript 2-3) to J2, including Xiaoquangou, Badaowan, Sangonghe, Xishanyao and Toutunhe age. The rivers and lakes sedimentary systems are good development. The rivers sedimentary systems are divided into braided stream and meandering stream.

结果 潮湿扇、河流和湖泊沉积体系是焉耆盆地的主要沉积体系类型,它们形成于中晚三叠世至中侏罗世的小泉沟、八道湾、三工河、西山窑和头屯河期;其中的河流沉积体系和湖泊沉积体系较为发育,河流沉积体系分为辫状河和曲流河两种类型。

Under experimental results of wax deposition and phase change, the mechanical characteristics of fluids flowing through porous media and the relevant physicochemical problem were all summed up as solving the gas-liquid-solid coupling mathematical model. After considering the phase change action between condensate gas and condensate liquid, wax deposition interlarded with interfacial drag force and capillary pressure engendered in the process of phase change. Numerical simulation results proved that the flow resistance increased and the production output decreased owing to wax deposition.

在蜡沉积变相态渗流实验和渗流数学模型的研究基础上,引入蜡沉积数学模型、考虑毛管力和表面张力的相对渗透率模型等,建立了相应的多孔介质中气-液-固变相态多相流-固耦合渗流数学模型,数值模拟结果表明,蜡沉积可使都分区域孔隙减少,流动阻力增大,不考虑蜡沉积会对产量预测明显偏大,蜡沉积可使产量下降。

On the basis of summarizing the status quotation of related researches at home and abroad, problems in related researches and studies are analyzed and the important research fields and contents in marsh sedimentology are chosen:Establishing different model of marsh sedimentation, to support marsh definition and classification from sedimentology; Advancing theory and quantification, to analyze formation process of marsh from quality to quantity methods; Applying modern sampling system and setting up standard sedimentation profiles; Strengthening the research of gleying marsh inland and its recent process and evidence derived from sedimentation profile; Enlarging geography fields and comparing between spatial and temporal research, and enforcing regional short timescale and highresolution environmental change; Paying much more attention on correlations between watershed environment and information derived from marsh sedimentary records and especially on their controlling mechanism.

主要从学术文献、权威机关与科研机构两个方面对相关的国内外研究现状和进展进行总结,针对国内外研究现状和存在的问题提出了今后研究的重点:建立不同成因的沼泽沉积环境模式,从沉积学角度对沼泽定义及分类提供支撑;注重理论提升与定量化,使沼泽形成过程分析从定性描述走向定量化;注重现代化采样系统的应用与标准沉积剖面的建立;加强内陆潜育沼泽研究,注重现代过程与沉积剖面证据;扩大地理覆盖面,加强时空对比,加强沼泽区域性短尺度、高分辨率环境演化研究;深化沼泽沉积信息与流域环境变迁耦合机制研究。

In this paper, a total of 56 relatively nonpoint source pollution sediment samples were collected from the tidal flats of the Jiuduansha shoal and the Chongming island of the Yangtze river estuary. The main properties i. e., grain size distribution, contents of DCB (dithionite citrate bicarbonate extracted iron Fe(subscript d, AAO extracted iron Fe(subscript o, total Fe, DCB extracted Mn Mn(subscript d, total Mn, organic matter, magnetic susceptibility of the samples, as well as the concentrations of Cu, Zn, Pb, Cr, Cd and Ni in the samples, were determined. Basing on the data, the relation of the sediment properties to heavy metal concentrations was evaluated with pearson's rank and partial rank correlation analysis.

采集长江口无明显点源污染的崇明东滩和九段沙潮滩56个沉积物样品,测定沉积物原样和粘粒中Cu,Zn,Pb,Cr,Cd和Ni的含量以及沉积物的主要性状(粒径分布、游离铁、活性铁、总铁、游离锰、总锰、有机碳和磁化率等),以相关分析和偏相关分析研究沉积物中重金属含量与沉积物主要性质之间的关系。

A Dense scale on the2O3(Cr/Y=4/1) coated specimen;2O3(Al/Y=3.6/1) coated specimen; Oxide nodules formed at the corner on the specimen coated with2O3(Cr/Y=2/1) deposited for 15 s; Locally spalled scale on the same specimen as in; The trace of cracks in the deposited oxide film on the scale formed on the specimen coated with2O3 (Cr/Y=2/1) deposited for 60 s; Showing the similar trace on the same specimen as in b

沉积复合OTFC试样的氧化层形貌有如下特征:(1)氧化层绝大部分致密、完整、与基体附着良好,晶粒细小(图7a,7b);(2)在短时间(15s)沉积2O3 OTFC试样的局部表面出现了不均匀氧化(图7c,7d),但只是在沉积Cr/Y=4/1膜试样的局部表面产生了类似无涂层Fe25Cr上剥落的厚膜(图7d);(3)沉积2O3(Cr/Y=2/1) 60s(图7e)与15s(图7c)的结果不同,前者整个试样表面氧化产物颗粒细小,无粗大氧化物颗粒形成;(4)沉积2O3(Cr/Y=2/1) 60s和2O3(Al/Y=3.6/1)薄膜的试样由于氧化增重非常少,氧化层很薄,刻印着涂层中局部出现的裂纹(图7e,7f),这种印迹的保留可能反映着传质机制的改变,即新氧化物由在外表面形成转变为在外表面以下形成。

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