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河流相层序地层
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  “河流相层序地层”译为未确定词的双语例句
     Discussion on the stratigraphic model in alluvial-fluvial facies sequence and its application in Jiyang depression.
     冲积—河流相层序地层模式探讨及其在济阳坳陷的应用
短句来源
     This paper studies the research method of sequence stratigraphy in fluvial facies by using high-resolution sequence stratigraphy relies on base-level cycle recognition.
     本论文以河流相沉积学研究为基础,运用以基准面旋回为参照面的高分辨率层序地层理论和研究方法分析了河流相层序地层单元的构成,探讨了河流相层序地层研究方法。
短句来源
     The principles of sedimentology and sequence stratigraphy were used to research the mode of sequence stratum of coastal alluvial environment. An universal mode for sequence stratum of alluvial-fluvial facies was established. The relationship between system tract and sedimentary facices was discussed on the analysis of river types of the Neogene in Jiyang Depression.
     运用沉积学及层序地层学原理 ,分析了河流类型及其形成发育特征 ,借鉴国内外有关冲积河流环境下的层序地层模式 ,特别是近海冲积环境下层序地层模式 ,并以济阳坳陷新近系为例 ,建立了更具普遍意义的冲积河流相层序地层模式 ,探讨了不同体系域的特征及其与河流类型之间的关系。
短句来源
     Study on Alluvial-Fluvial Facies Sequence Stratigraphy and Favorable Reseivoir Zones Prediction for Neogene, Inshore Area, Jiyang Depression
     济阳坳陷滩海地区新近系冲积-河流相层序地层研究与有利成藏区带预测
短句来源
     THE MODE OF SEQUENCE STRATUM OF ALLUVIAL-FLUVIAL FACIES--TAKING THE UPPER TERTIARY OF JIYANG DEPRESSION FOR EXEMPLE
     冲积-河流相层序地层模式——以济阳坳陷新近系为例
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  相似匹配句对
     Characterization of Sedimentology in Fluvial Facies Reservoir
     河流储层沉积学表征
短句来源
     Fluvial Facies Sequence Stratigraphy Discuss
     河流层序地层学研究
短句来源
     FLUVIAL FACIES MODEL AND HETEROGENEITY OF FLUVIAL RESERVOIRS
     河流模式与储层非均质性
短句来源
     STUDY ON ALLUVIAL-FLUVIAL FACIES SEQUENCE STRATIGRAPHY
     冲积-河流层序地层学研究
短句来源
     Architecture Model of Sequence Stratigraphy in Fluvial Facies
     河流层序地层构成模式探讨
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Asluvial structures of fluvial facies are affected by each effect between supplying of taliment and pnducing of accommedately room. The recognition of their Sequence and systern tract is according to situation of piling up of channel sand they and develoPment of palesoil or nuvial type: no recod of sediment in the early LST and braided stream in the later LST, meandeting stream and anastomosing strearn in TST, meandering strearn in HST, braided strearn in the Rar.

河流相的层序地层结构是由沉积物的供给和可容纳空间之间的相互作用决定的,其居序与体系域的识别和划分则是根据河道砂体的叠置方式及相伴生的古土壤的发育情况或河流类型来进行的,低水位早期主为侵蚀下切无沉积记录,低水位晚期主为辩状河;水进时期先为曲流河、后为网状河;高水位时期为曲流河,水退时期主为辩状河。

The principles of sedimentology and sequence stratigraphy were used to research the mode of sequence stratum of coastal alluvial environment. An universal mode for sequence stratum of alluvial-fluvial facies was established. The relationship between system tract and sedimentary facices was discussed on the analysis of river types of the Neogene in Jiyang Depression. The results show that there are four types of system tracts in alluvial-fluvial facies including low system tract, extension system tract, high...

The principles of sedimentology and sequence stratigraphy were used to research the mode of sequence stratum of coastal alluvial environment. An universal mode for sequence stratum of alluvial-fluvial facies was established. The relationship between system tract and sedimentary facices was discussed on the analysis of river types of the Neogene in Jiyang Depression. The results show that there are four types of system tracts in alluvial-fluvial facies including low system tract, extension system tract, high system tract, contracting system tract. According to the sedimentary characteristics of the Neogene in Jiyang Depression, the types of sediment system and facies corresponding to the different system tracts were given. There were alluvial-braided river facies in low system tract. The braided river was transited to meandering river in extension system tract. There was meandering river in the high system tract, and the meandering river was transited to braided river in the contracting system tract.

运用沉积学及层序地层学原理 ,分析了河流类型及其形成发育特征 ,借鉴国内外有关冲积河流环境下的层序地层模式 ,特别是近海冲积环境下层序地层模式 ,并以济阳坳陷新近系为例 ,建立了更具普遍意义的冲积河流相层序地层模式 ,探讨了不同体系域的特征及其与河流类型之间的关系。研究结果表明 ,冲积河流相地层的体系域划分具有 4分性特征 ,即主要发育有低水位体系域、扩张体系域、高水位体系域 ,当基准面缓慢下降时 ,还可发育收缩体系域。根据济阳坳陷新近系沉积特征 ,指出了各体系域对应的沉积体系及相类型。其中 ,低水位体系域时期以侵蚀下切、冲积扇辫状河沉积为主 ;扩张体系域时期是由辫状河向曲流河过渡 ;高水位体系域时期以曲流河为主 ;收缩体系域时期是由曲流河向辫状河过渡。

Fluvial facies stratum is one of important reservoirs in Meso-Cenozoic continental basin in China. Sequence stratigraphy conventional sequence stratigraphy interpretation techniques based on seismic stratigraphy in passive continental margin is generally considered difficult to be applied to fluvial facies due to the sequence complexity and multiple mixed facies. The paper studies sequence architecture of fluvial strata by using high-resolution sequence stratigraphy based on base-level cycle recognition. Geological-seismic...

Fluvial facies stratum is one of important reservoirs in Meso-Cenozoic continental basin in China. Sequence stratigraphy conventional sequence stratigraphy interpretation techniques based on seismic stratigraphy in passive continental margin is generally considered difficult to be applied to fluvial facies due to the sequence complexity and multiple mixed facies. The paper studies sequence architecture of fluvial strata by using high-resolution sequence stratigraphy based on base-level cycle recognition. Geological-seismic response models of fluvial reservoirs have been established, which are also illustrated by an example in Guantao Formation, Upper Tertiary, Offshore area in Shengli Oilfield.

冲积—河流相是我国中、新生代陆相盆地重要油气储集层系类型之一。由于河流相层序地层成因和相构成的复杂性 ,以被动大陆边缘地震地层学研究为基础、以三分体系域构成为地层预测模式的经典层序地层学分析方法并不一定适合河流相储层。本文以河流相沉积学研究为基础 ,运用以基准面旋回为参照面的高分辨率层序地层理论和研究方法分析了河流相层序地层单元的构成 ,建立了主要储层的地质—地震解释模型 ,并以胜利油田垦东地区上第三系馆陶组为例说明河流相层序构成特征和地质—地震解释方法。

 
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