准噶尔盆地乌尔禾地区风城组致密油储层成因分析——来自岩石组分、结构构造和稀土元素的证据
首发时间:2016-05-03
摘要:下二叠统风城组是准噶尔盆地西北缘乌尔禾地区勘探潜力巨大的非常规致密油储层,但目前对此类致密油储层的成因尚不清楚,制约着风城组致密油藏的勘探开发效益。研究表明,该致密油储层的物质组分极其复杂,不仅富含白云石、(含)铁白云石和火山凝灰物质及少量陆源碎屑,同时富含硅硼钠石、水硅硼钠石、碳酸钠钙石、碳钠镁石、碳氢钠石、氯碳钠镁石、天然碱、石盐、石膏等复杂盐类矿物为显著特征,并且广泛发育由各种白云石、火山凝灰物质和复杂或单一的盐类矿物组成的纹层状、条带状、网脉状、同生变形和喷爆角砾等结构构造,与国内外已公布的海相和陆相"白烟型"喷流岩的物质组成大相径庭,但常见的典型热水沉积结构构造基本一致,因此,将风城组致密油储层的成因归属为物质组分极其特殊的湖相 "白烟型"喷流岩。稀土元素地球化学特征的研究,不仅表明风城组致密油储层成因与同期火山岩的脉动式喷发活动有关,而且热液喷流和物质组分的供给与同期喷发的安山岩具有亲缘性,特别是由风城组喷流岩的Ce、Eu异常,进一步反映热液喷流的沉积作用发生在半深湖-深湖底强还原环境的热卤水池中,与火山岩喷发活动有关的热液喷流具有中-低温强碱性热卤水性质。
关键词: 岩石学 致密油储层 白烟型喷流岩 岩石组分 稀土元素 下二叠统风城组 准噶尔盆地
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Genesis of Tight Oil Reservoir in Lower Permian Fengcheng Formation in Urho Area, Junggar Basin—Evidence from the Components, Structures and Rare Earth Element
Abstract:Lower Permian Fengcheng Formation is a kind of unconventional tight oil reservoir with great exploration potentials in northwestern margin of Junggar Basin. The genesis of this type of reservoir is not clear until now, so the exploration and development benefit is confined. Researche shows that the composition of this tight oil reservoir is extremely complicated, contains not only dolomite, ferroan dolomite or ferrodolomite, tufaceous and terrigenous clast, but also complex saline minerals such as reedmergnerite, searlesite, shortite, eitelite, wegscheiderite, northupite, trona, halite and gypsum. Hydrothermal sedimentary structures and textures such as dolomite,tufaceous, complex or single saline minerals lamellar or banded, veined-network, contemporaneous deformation and eruptive breccia are widely distributed. Mineral composition of this reservoir is different from marine or continental facies"white smoke type"exhalative rock published home and abroad, but the structures and textures are accordance with them. So we classify this kind of tight oil reservoir in Fengcheng Formation to lacustrine "white smoke type" exhalative rock with special mineral composition. Research about REE show that the formation of this tight oil reservoir is closely related to contemporaneous pulsatile eruption of volcanic rocks, and the affinity between source of hydrotherm and mineral composition and andesite is strong. The Ce and Eu anomaly in Fengcheng Formation indicate that the sedimentation of hydrotherm proceeded in deep-semideep lacustrine hot brine pool with reducibility. Property of hydrotherm related to volcanic eruption is mid-low temperature, strong alkaline hot brine.
Keywords: petrology tight oil reservoir “white smoke type” exhalative rock rock components rare earth element Lower Permian Fengcheng Formation Junggar Basin
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准噶尔盆地乌尔禾地区风城组致密油储层成因分析——来自岩石组分、结构构造和稀土元素的证据
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