• 这些气源岩主要为浅湖—深湖沉积产物;

    These source rocks mostly are sediment of shore lake-shallow lake;

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  • 自下而上由浅湖相、三角洲相和曲流河相组成。

    From bottom to top, it consists of shallow lacustrine facies, delta facies and meandering river facies.

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  • 阿尔善沉积时期湖水范围较小,以滨浅湖为主。

    During Aershan depositional period, the lake range was rather smaller and shore-shallow lake facies is the main characteristic.

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  • 研究区储集层岩相主要为三角洲相、滨浅湖相砂体。

    The reservoir types in the studied region are mainly deltaic facies and inshore shallow lake facies sand bodies.

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  • 主要沉积体系为河流、三角洲、冲积扇及滨浅湖相。

    The main sedimentary system includes fluvial, delta, alluvial fan and lake facies.

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  • 可划分为滨线-浅湖、辫河浅湖-深湖和风积三种沉积形态。

    They are divided into three sediment formations, shoreline-shallow lake, braid lake-deep lake and wind deposition.

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  • 研究层段主要发育于滨浅湖亚环境,形成的微相以滩坝微相为主。

    The clastic rocks of investigative area mainly developed in shoreside and shallow lake. The microfacies mainly included beach and bar.

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  • 高位体系域主要发育滨浅湖相、河流相及进积型三角洲沉积体系。

    Highstand System Tract mainly develops depositional system of offshore-meare, fluvial facies and prograded delta.

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  • 生烃组合分为烛藻煤深湖相泥岩和腐殖煤烛煤浅湖相泥岩两种类型。

    The hydrocarbon generating assemblage can be divided into two types of cannel boghead deep lake mudstone and humic coal cannel coal shallow lake mudstone in this basin.

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  • 布罗兹区的浅湖连接着六条河流,形成了一个往来自由通行无阻的水路航行系统。

    Six rivers link the Broads' shallow lakes, creating a lock-free, navigable system of waterways.

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  • 认为沙市组是形成于半干旱气候条件下的浅湖陆源碎屑岩和盐湖沉积。

    It shows that Shashi Formation composite of shallow lacustrine and continent source clastic rock and salt deposits that sedimented and developed in the half draught climate.

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  • 措勤盆地唢呐湖组以陆湖泊相为主,划分为扇三角洲、滨湖相和浅湖相。

    The Cuoqin basin Suonahu Formation is lacustrine facies and been divided into fan-delta and shallow lagoon facies.

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  • 嫩一段和嫩二段主要发育滨—浅湖和半深—深湖沉积,零星分布薄层砂滩砂体。

    The shore-shallow lake and hemi-deep-deep lake develop in the first and second member of Nenjiang formation, and thin bed beach sands distribute fragmentarily.

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  • 合川地区须二段处于滨浅湖亚相环境,滨浅湖滩坝砂体是该区主要的储集砂体。

    The sedimentary environment of the 2nd member of the Xujiahe Fomation is shore-shallow lacustrine. The reservoir sand is beach bar.

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  • 高水位体系域主要由滨浅湖沉积体系、扇三角洲沉积体系和浊积扇沉积体系组成。

    High stand system tract is composed of coast and shallow lake sedimentary system, fan delta sedimentary system and turbidite fan sedimentary system.

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  • 识别出扇三角洲、远(近)源三角洲、水下扇及浅湖、深湖-半深湖等沉积体系。

    The sedimentary systems in the T-R cycle: fluvial fan, fan delta, common delta and lacustrine sedimentary system.

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  • 其中沿最大湖岸线带状分布的富62井—富13井一带的滨浅湖砂质滩坝规模较大。

    The distribution of zonary shore-shallow lacustine sandy beach-bars along the maximum lacustine bank line in the area of Fu 62 well-Fu 13 well is bigger.

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  • 碳酸盐岩沉积相可划分为滨湖灰泥坪、滨湖藻坪、浅湖颗粒滩、浅湖藻丘以及半深湖泥灰岩相。

    Carbonate sedimentary facies include lime-mud flats and algal flats in littoral lake, grain banks in shallow lake, algal mounds in shallow lake and marls in semi-deep lake etc.

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  • 其中滨湖亚相的岸滩微相为主要的有利储集相带,浅湖亚相的浅滩微相属于较有利的储集相带。

    And the beaches in the lakeside are main advantageous accumulation, the shoal in shallow belongs to the advantageous store to bring.

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  • 已经变成了浅湖的泛滥河道偶尔还会因洪水而再度溢满,风景如画的美丽湖泊于是成为了鱼类的天下。

    Overflow channels that have become shallow lakes, periodically recharged with water and fish by the floods, pattern the landscape.

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  • 在纵向上,从E31 -E32,从下向上由辫状河三角洲相变为浅湖相,构成了一正旋回沉积。

    In vertical, from E31 to E32, it changes from braided river delta to a shallow lake facies, thus, formed a cycle which lithologic character is rough at bottom.

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  • 沉积相总体特征以滨浅湖沉积为主,而在研究区周缘则多发育河流泛滥平原、三角洲和扇三角洲沉积。

    The general sedimentary characteristics indicate that shore-shallow lacustrine deposits are the main types, while flood plain, delta and fan delta occurred mainly along the basin margin.

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  • 英格兰东部的低地地区,有大片宽广的浅湖,与河流和小溪交错。布罗茨是野生生物保护区和娱乐中心。

    A low-lying region of eastern England with wide, shallow lakes interconnected by rivers and small streams. The Broads is a wildlife sanctuary and recreational center.

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  • 四川盆地西部侏罗系沙溪庙组是河流—三角洲—滨浅湖沉积为主的红色砂泥岩系,天然气资源相当丰富。

    Abundant in natural gas sources, Jurassic Shaximiao Formation in west Sichuan Basin is a red sandstone and shale mainly deposited in fluvial, deltaic shoal faces.

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  • 形成了冲积扇—扇三角洲—滨浅湖泊、三角洲前缘—滨浅湖—中深湖、中深湖—浅湖沉积体系组合型式。

    It formed such association types as alluvial fan-fan delta-shallow coastal lake, delta front-shallow coastal lake-semi-deep lake, semi-deep lake shallow lake sedimentary system.

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  • 文留油田文65块发育水下分流河道、水下分流河道侧翼、水下天然堤、水下分流间湾、滨浅湖泥5种微相。

    Five microfacies of subsea distributary channel, its flank, subsea natural barrier, subsea interdistributary bay and coastal or neritic shale are developed in Block Wen 65 of Wenliu Oilfield.

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  • 在此基础上建立了滨浅湖沉积环境下不同沉积微相的储层非均质性模式,为油田开发方案的编制和调整打下基础。

    On this base we build a mode of reservoir heterogeneity of Shore-lake and Shallow-lake sub-facies. The results is helpful to the research of reservoir and adjusting production of oilfield development.

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  • 在此基础上建立了滨浅湖沉积环境下不同沉积微相的储层非均质性模式,为油田开发方案的编制和调整打下基础。

    On this base we build a mode of reservoir heterogeneity of Shore-lake and Shallow-lake sub-facies. The results is helpful to the research of reservoir and …

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  • 在此基础上建立了滨浅湖沉积环境下不同沉积微相的储层非均质性模式,为油田开发方案的编制和调整打下基础。

    On this base we build a mode of reservoir heterogeneity of Shore-lake and Shallow-lake sub-facies. The results is helpful to the research of reservoir and …

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