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Characteristics of Salt Lake Deposition and Significance for Oil-gas Exploration of Xingouzui Formation, Xingou oilfield, Jianghan Basin

机译:江汉盆地兴某油田盐湖沉积特征及石油天然气勘探的意义

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Jianghan Basin is a typical Mesozoic-Cenozoic salt lake basin of East China, oil and gas reservoir with industrial utilization value was found in the Xingouzui Fm, Xingou Oilfield of this basin, the formation of which is closely related to the dolomite stratigraphy deposited in the salt lake. In order to explore the relationship between salt lake deposition with oil-gas reservoir and to get better understanding of the character of Jianghan Basin Salt Lake deposit to provide theoretical foundation for the exploration and development of the oil and gas resources. This paper, based on the elaboration study of the layer section core, combined with detection logging information and analysis test data, describes the salt lake deposit character according to the salt mineral species and profile thickness, makes an analysis of its formation mechanism, and discusses the salt lake deposit's indicating significance toward paleoclimate. The result suggests that the salt lake deposit of the research area demonstrate obvious feature of rhythmicity. Which shows in the alternating appearance of rhythmite composed by mudstone, dolomite, gypsum and rock salt. This kind of rhythmicity is a direct response of constantly changing of lake level rising-falling. The wide development of eury-thermal saline minerals such as calcite and dolomite, indicates that the palaeoclimate was arid to semi-arid in Jianghan Basin during the deposition of Xingouzui Formation in Paleogene. A complete salt rhythm can form a source-reservoir-seal assemblage, which has an important meaning for hydrocarbon generation, accumulation and preservation.
机译:江汉盆地是一家典型的中生代新生代盐湖湖盆地华东,石油和燃气藏具有工业利用价值,在邢友富芒,本盆景油田,其形成与白云岩地层沉积密切相关盐湖。为了探讨盐湖沉积与油气藏的关系,以了解江汉盆地盐湖矿床特征,为石油和天然气资源勘探开发提供理论基础。本文基于层段核心的精细研究,与检测测井信息和分析试验数据相结合,描述了盐湖沉积物,根据盐矿物物种和型材厚度,对其形成机制进行了分析,并讨论盐湖沉积物对古古典的意义表明。结果表明,研究区的盐湖矿床展示了节奏性的明显特征。这在泥岩,白云石,石膏和岩盐组成的节奏的交替外观中。这种节奏性是湖泊水平上升落下的不断变化的直接反应。盐酸和白云石等鳗鱼热盐矿物的广泛发展表明,在古雄Xingouzui形成期间,古典气候在江汉盆地在江汉盆地进行了干旱。完整的盐节律可以形成源 - 储层 - 密封组件,其对碳氢化合物产生,积累和保存具有重要意义。

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