三角洲前缘
- 网络delta front;delta-front
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GA层段顶部的地震振幅异常呈分散块状(河口砂坝)和弯曲带状(分流河道间三角洲前缘);
The top of the GA interval shows patchy ( mouth bar deposits ) and curvilinear ( interdistributary delta front ) seismic amplitude anomaly .
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储层为致密砂岩储层,平均孔隙度4.74%,渗透率0.417×10-3μm2;有利的储层微相是三角洲前缘水下分流河道、河口砂坝;
The reservoirs are tight sand , with an average porosity of 4 . 74 % and permeability of 0 . 417 × 10-3 μ m2 . Delta front underwater distributary channel and mouth bar are the favorable reservoir micro-facies .
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Ⅶ油组以下(N1)主要为辫状河三角洲前缘-滨浅湖沉积;
Below VII oil measure ( N1 ) is dominated by braided stream delta front-shore saucer lake deposits ;
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通过应用倾角散射程度与沉积环境的关系,对B凹陷沉积特征和物源方向进行了分析,得出B凹陷是受2条主河道控制的扇三角洲前缘辫状河道沉积;
According to the relationship between dip scattering strength and depositional environment , the deposition characteristic and the sand source direction of depression B were analyzed . The depression B is the deposition of a fan delta with braided river course which is controlled by two main rivers .
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其中在C17n·3n极性亚期内,最大沉积速率可达220.2mm/ka。这主要发生在三角洲前缘的沉积物卸载区。
And the most deposital velocity was 220.2mm/ka during C17.3n sub-period , which mainly occurred at the unloaded area in the front of the delta .
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进入河口区的泥沙约884%堆积在水下8km宽的三角洲前缘。
More than 88.4 % of the suspended silt into the river mouth area is deposited on the delta front slope of average 8 km in width .
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II油组沉积时期具有近物源、粗碎屑、小水系的特征,工区位于扇三角洲前缘的朵体之上,物源来自NNE&NEE向(30~85o)。
From depositional view , oil set II is featured by close provenance , coarse grain , and short water system . The studied area lies on one lobe of fan-delta front , and its provenance is from the NNE or NEE ( 30 ~ 85o ) .
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三角洲前缘(水下分流河道相和河口坝相);
) delta front ( subaqueous channel and mouth bar fades );
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坳陷湖盆三角洲前缘储层砂体成因研究
Genetic research of reservoirs at delta front in depressed lacustrine basins
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不平坦的三角洲前缘席状砂&来自露头和地下的证据
Non-flattening Delta Front Sheet Sand & Evidence from Outcrops and Subsurface
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三角洲前缘的水下分流河道砂岩为最优质的储集层。
Subaqueous distributary channel sandstones of delta front are fine reservoir .
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扇三角洲前缘亚相由近端坝和远端坝沉积组成。
Fan delta front includes proximal and distal bar deposits .
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浅水三角洲前缘平坦、开阔。
Shallow - water delta front is flat and widen .
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优质储集层主要分布在三角洲前缘水下分流河道微相中。
The favorable reservoir mainly distributes in the delta-front submarine distributary channel .
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坳陷湖盆三角洲前缘沉积微相构成及其分带性
The Microfacies Architecture and Zoning of Delta Front in Depressed-type Lacustrine Basin
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整个研究区为三角洲前缘。
All the study area were delta front sedimentary system .
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长期基准面下降半旋回主要由滨浅湖→三角洲前缘构成。
Its falling semi-cycle mainly consists of shore-shallow lake → . delta front .
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沉积相是最主要的因素,三角洲前缘水下分流河道砂体是主要的储集体。
Major reservoir is sand bodies of subaquatic distributary channels in delta fronts .
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其中三角洲前缘水下分流河道为骨架相。
Among them , underwater distributary channel in delta front was the main facies .
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三角洲前缘砂体骨架的随机模拟
Stochastic modeling of sand framework of deltaic front
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三南凹陷中西部地区和基东鼻凸是勘探的有利区带,有利相带为三角洲前缘水下分流河道及前缘滑塌体。
Subsea divided flow fluvial channel and slip block of delta front are favourable zone .
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从成因类型上看,三角洲前缘砂体包括:(1)水下分流河道砂体;
The delta front sand stones include ( 1 ) subaqueous distributary channel sand stone ;
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扇三角洲前缘地质知识库的建立及应用
Development and application of geological knowledge database for fan-delta front in the dense spacing area
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北部发育三角洲前缘沉积。
Delta front occurred in the north .
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相反,形态规则、保存完好的三角洲前缘反而不利于滑塌浊积岩的形成。
In contrast , the regular and good reserved delta front is disadvantaged to form fluxoturbidite .
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扇三角洲前缘,包括水下分支河道、河道间沉积及滨岸和席状砂沉积;
Fan-delta front , including underwater dis-tributary channel , inter-channel , shoreline and sheet-like sand sediments ;
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三角洲前缘韵律层特高含水期剩余油分布及调整
Residual oil distribution and reconciliation for delta front rhythm zone in extra high water cut stage
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三角洲前缘亚相在MSCZ1都有存在,微相以水下分流河道和河口坝为主,其次为远砂坝微相。
Micro-phase are mainly underwater distributary channel and mouth bar , followed by the distal bar facies .
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各旋回中的扇三角洲前缘亚相和水下扇扇中亚相是较好的储集相带。
Fan delta front subfacies and subaqueous medium fan subfacies of every cycle are good reservoir facies .
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葡北油田四断块葡Ⅰ油组三角洲前缘储层结构特征研究
Reservoir Architecture Characteristics of Delta Front of Pu I Oil Group in Block 4 , Pubei Area