1) Braided Delta
辫状三角洲
1.
Analysis of sedimentary system and intercalation characteristics of braided delta: A case study of Anfeng in Hai'an depression;
辫状三角洲沉积体系夹层分布特征研究——以海安凹陷安丰辫状三角洲为例
2.
Deposition systems and reservoir properties of Xinzhuang braided delta in Biyang Depression;
泌阳凹陷新庄辫状三角洲沉积体系及储集性能
3.
Sedimentary mode and formational structure analysis in Anfeng retrograding type braided delta of Hai’an depression;
海安凹陷安丰退积型辫状三角洲沉积模式及建筑结构分析
2) braid delta
辫状三角洲
1.
The research indicated that the front surfacies of braid delta has been recognized in Third group of Member L-3 and five sedimentary micro-facies have been distinguished as follows: subaqueous distributaries river course,interdistributary bay,river mouth bar,distal bar and subaqueous natural levee.
研究表明,W-1油田L-3段Ⅲ油组为辫状三角洲的前缘亚相沉积,主要发育水下分流水道、分流水道间、河口砂坝、远砂坝及水下天然堤等5种微相类型。
2.
A braid delta is an important type of lacustrine deltas.
笔者对辫状三角洲的沉积特征、储集性能进行了详细的描述 ,并对其分类进行了探讨。
3) braided channel and braided delta deposits
辫状河与辫状三角洲
4) sandbody of braide river-delta
辫状三角洲砂体
5) braided river delta
辫状河三角洲
1.
Characteristics of Paleogene braided river delta deposits in Gudong area;
孤东地区古近系辫状河三角洲沉积特征
2.
Construction of geologic model for lithologic oil reservoirs in braided river delta with sequence stratigraphy;
用层序地层学构建辫状河三角洲岩性油藏地质模型
3.
Sedimentary characteristics of the shallow Jurassic braided river delta,the Junggar Basin;
准噶尔盆地侏罗系辫状河三角洲沉积特征
6) braided delta
辫状河三角洲
1.
Sedimentary characteristics of the braided deltas in the eighth member of the Lower Shihezi Formation in the northeastern part of the Ordos Basin;
鄂尔多斯盆地东北部下石盒子组盒8段辫状河三角洲沉积特征
2.
The deposition of braided deltas:an example from the Zhujiatai Formation in the Minhe Basin,northwestern China;
一个辫状河三角洲的沉积特征——以民和盆地朱家台组为例
3.
It is held that E_2S_1~6 reservoir zones in this area are a set of braided delta sedimentation, which deposited under the background of lake recession.
以岩心观察及分析资料为基础 ,结合测井、录井和油田动态资料 ,研究了真武油田垛一六油组的沉积相类型、微相组成以及主要沉积微相的特征 ,认为该区垛一六油组为一套湖退背景下形成的辫状河三角洲沉积 ,底部的 C5单元为辫状河三角洲前缘及前辫状河三角洲沉积 ,上部 C1～ C4单元为辫状河三角洲平原沉积 。
补充资料：岛屿状三角洲
其形成一般是通过河口心滩——分汊——沙岛发展而成，星罗棋布的沙洲和沙岛和纵横交错狭长的汊河构成三角洲平原的主体。如恒河三角洲、珠江三角洲。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条