• 泌阳凹陷南襄盆地中的一个次级凹陷

    Biyang depression was a secondary depression in Nanxiang Basin.

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  • 泌阳凹陷斜坡断层发育断裂系统复杂

    The slope zone of Biyang depression developed many faults and has complicated faults system.

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  • 泌阳凹陷北部斜坡具有优越油气富集条件

    Favorite conditions for oil enrichment exist in the Northern Slope zone of Biyang depression.

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  • 泌阳凹陷北部斜坡带发育两种类型三角洲

    There are two kinds of deltas in the Northern Slope of Biyang Depression.

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  • 研究成果泌阳凹陷中南部地区勘探取得明显效果

    The results have been applied in the second time exploration in the center and south part of biyang depression.

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  • 泌阳凹陷双河油田中国东部大型构造-岩性复合油藏之一。

    Shuanghe oilfield in Biyang depression is one of the large structural-lithologic composite oil reservoirs in eastern China.

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  • 中国大陆河南省驻马店市泌阳邮政编码463700。

    The postcode of Miyang County, Zhumadian City, Henan Province, China is 463700.

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  • 论文主要关于泌阳凹陷东南边沿带地震采集方法研究

    This dissertation is a study on 3D seismic acquisition method in south-east area of Biyang depression.

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  • 因此泌阳凹陷复杂鼻构造具备形成大面积油气富集区地质条件

    Therefore, the complex fault block groups in Biyang depression have the geological conditions to form large hydrocarbon enrichment areas.

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  • 南襄盆地泌阳凹陷南部陡坡不同地区发育不同类型隐蔽油气藏

    The southern steep slope zone in the Biyang Sag of the Nanxiang Basin, is characterized by various categories of subtle hydrocarbon reservoirs.

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  • 泌阳凹陷南襄盆地中的次级构造单元,为一超式状凹陷。

    Biyang depression is a secondary structural unit in Nanxiang Basin. The depression is in half-graben shape which faulted in the south part and overlapped in the north part.

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  • 应用层地层学沉积体系分析方法,建立泌阳凹陷地层单元

    By using the analytical method of sequence stratigraphy and sediment system, an isochronous unit of Biyang Depression was established.

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  • 泌阳凹陷一个新生代断陷盆地岩性变化,断裂发育,油藏类型

    Miyang Depression is a Mesozoic-Cenozoic fault basin, where lithologic change is fast, fault is developed, reservoir type is various.

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  • 泌阳凹陷的油气田环带状分布沉积渗入锋面位置压力平衡带上。

    Oil and gas reservoirs in Biyang depression distribute in circularity in the pressure equilibrium zone on the frontal surface between sedimentary water and infiltration water.

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  • 泌阳凹陷新庄地区油层埋藏厚度富集程度,油藏类型鼻断块油藏为主

    Reservoirs in Xinzhuang area, Biyang depression, are characterized by shallow burial depth, large thickness and high enrichment, and are mainly of fault-nose and fault-block types.

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  • 泌阳断陷陆相外部构型研究包括层序级别的厘定与划分以及界面的类型及其识别标志

    The study on the outer configuration of terrigenous sequence in Biyang fault depression includes sequence classification and boundary identification.

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  • 泌阳沉积了巨厚的老第三系稳定的湖相水下沉积,主要生油区,地层极平缓。

    The layers in the deep depression which was the main oil source area are almost horizontal.

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  • 泌阳断陷沉积了巨第三系稳定的相水下沉积,主要的生油区,地层极平缓。

    There is great thickness of lake sediments of Eogene in Biyang rifted-basin. The layers in the deep depression which was the main oil source area are almost horizontal.

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  • 泌阳凹陷在区域性作用形成典型的伸展构造样式——不同层次断层切割一系列复杂、断

    Typical extensional structural patterns, cut into a series of complex fault noses and fault blocks by faults of different levels, form under regional extension force in Biyang depression.

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  • 深入研究泌阳凹陷大量岩心测井地震资料基础上,证实泌阳凹陷具有独特的盆地结构样式和形成机制

    Detailed studies of a number of core sections, well logs and seismic data of the Biyang depression reveal that the depression had a special construction style and forming mechanism.

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  • 近些年国内生产、社会经济形势的影响,各地肉牛总体存栏量逐年减少,泌阳肉牛存栏量减少情况非常明显。

    Inrecent years, affected by domesticproduction, social and economic situation, aroundthe overall amount of beef cattle herdsreduced year by year, Biyang County reduction is also veryobvious.

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  • 结果表明泌阳湖盆沉积充填划分个阶段:初始断陷充填阶段、断陷充填阶段及坳充填阶段,并分别对应着三个构造层序。

    The result shows that sediment filling history of Biyang fault depression can be classified into initial rift, main rift and downwarp filling stages which have in turn formed three tectonic sequences.

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  • 结果表明泌阳湖盆沉积充填划分个阶段:初始断陷充填阶段、断陷充填阶段及坳充填阶段,并分别对应着三个构造层序。

    The result shows that sediment filling history of Biyang fault depression can be classified into initial rift, main rift and downwarp filling stages which have in turn formed three tectonic sequences.

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