crevasse channel

[kriˈvæs ˈtʃænl]
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    决口水道

数据更新时间:2026-06-10 14:59:31
1、

Shanxian formation is old crevasse splay and old channel sedimentary of the Yellow river, and its propery is mainly fine silt and silt;

单县组为黄河古决口扇、古河道沉积,岩性主要为细砂、粉砂;

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2、

E. meandering point bars, crevasse splays, natural levees and flood plains. CHANNEL GEOMETRY OF ALLUVIAL STREAMS

曲流河相自下而上为河床滞留沉积-点坝-天然堤-决口扇-泛滥平原的正韵律组合。冲积河流的河相关系

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3、

In the third stage ( Shanxi Age), swamp, distributary channel, natural levee and crevasse splay occurred alternatively.

第三阶段(山西组)河道、沼泽、天然堤、决口扇环境交替出现;

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4、

distributary channel inter distributary bay deposit, crevasse channel are developed in the strata of fuyu oil-bearing layer.

扶余油层在研究区属三角洲平原亚相沉积,主要发育了以下微相类型:分流河道、分流间湾和决口河道。

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5、

It divided into point bar, the last channel, abandoned channel, crevasse splay, spill shore sand, flood plain six kinds of sedimentary microfacies.

划分为点坝、末期河道、废弃河道、决口扇、溢岸砂、泛滥平原6种沉积微相。

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