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坡折带是沉积地貌突变的古构造枢纽带。The slope-break zone is a pivotal zone of depositional physiognomy.

蓝田组沉积环境演化旋回性明显,由两个完整的旋回组成。Evolution of depositional environment of LF includes two entire cycles.

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动物群落与沉积环境有直接关系。Faunal assemblage are directly related to the depositional environment.

总结了研究区下切谷和辫状河三角洲的沉积模式。Depositional models of the incised valley and braid delta were summed up.

在伸展断陷盆地内均有明显的沉积响应。There were obvious depositional response in the extensional faulted basin.

台北凹陷在侏罗纪以后成为吐哈盆地的沉积中心。Taibei Say was the depositional center of Turpan-Harmi Basin after Jurassic.

同时,而且对应于基准面的变化,河流存在着复杂的沉积响应方式。Rivers often have complex depositional modes corresponding to the base-level changes.

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控制储层发育的主要因素是成岩作用和沉积相、沉积微相。The main factors controlling the reservoir quality are diagenesis and depositional facies.

研究区内存在冲积扇、曲流河、扇三角洲、湖泊等相类型。Under this depositional setting, alluvial fan, river, fandelta and lake facies are developed.

沉积基准面旋回变化控制着陆相层序地层的形成与演化。Depositional base-level cycle controls the development and evolution of sequence stratigraphy.

传统的煤沉积模式难以解释其超厚煤层的成因。Traditional coal depositional model can hardly explain the cause of this extra-thick coal seam.

沉积相的分布格局控制着砂体类型和分布。The distribution configuration of depositional system controlled the sand types and distribution.

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流沙港组主要发育辫状河三角洲相和湖泊相两种沉积体系。Braided delta and lacustrine facies are two major depositional systems developed in Liushagang Fm.

长江水下三角洲是一个以径、潮流相互作用为主的沉积体。The subaqueous Changjiang River delta has its own distinctive depositional processes and products.

下切谷是准噶尔盆地西缘车排子地区的一种重要沉积体系。Entrenched valley is an important depositional system in Chepaizi area in the west of Junggar Basin.

文章描述了上述各深水环境相特征。The facies characteristics of above-mentioned depositional environments are described in this paper.

该侵蚀盆地于中晚更新世闭合并演化成一个独立的沉积盆地。This erosional basin was closed and evolved into a depositional basin during middle Late Pleistocene.

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结果表明,降雨过程中有两种类型结皮形成,即沉积结皮和结构结皮。Two kinds of crust, i. e. , structural crust and depositional crust, were observed in the experiment.

白云凹陷是新生代在伸展性大陆边沿上发展起来的大型沉积盆地的一个次级构造单元。Baiyun depression is part of large depositional basin on the edge of extensional continent in Cenozoic.

综合分析认为,引起储层非均质性的主要原因是沉积环境的变化。By analyses, the main reason of poor reservoir heterogeneity is the change of depositional environment.