煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2013年
6期
1-6
,共6页
潘松圻%庄新国%王小明%张杰%唐辉
潘鬆圻%莊新國%王小明%張傑%唐輝
반송기%장신국%왕소명%장걸%당휘
准东煤田%西黑山勘查区%层序地层%沉积相%显微组分%煤相
準東煤田%西黑山勘查區%層序地層%沉積相%顯微組分%煤相
준동매전%서흑산감사구%층서지층%침적상%현미조분%매상
eastern Junggar coal field%Xiheishan area%sequence stratigraphy%sedimentary facies%maceral%coal facies
运用层序地层原理,通过岩心和测井资料的综合分析,对新疆准东煤田西黑山勘查区西山窑组进行了层序地层研究,识别出3个体系域-)-低位、湖扩和高位体系域,并进一步进行了高频层序单元的划分。在层序地层格架的约束下,分析了西山窑组沉积体系的配置关系,识别出辫状河三角洲和湖泊沉积体系,进而细分为4个亚相和8个微相类型。同时,对煤岩样品进行了煤质分析和显微组分定量统计,确定了研究区煤相类型主要为潮湿森林沼泽相和干燥森林沼泽相。该区煤相的垂向演化规律受湖平面升降变化所控制,而湖平面的升降受层序地层格架的约束,在不同体系域中湖平面的变化控制泥炭沼泽的发育,从而决定了煤质煤相的演化规律。
運用層序地層原理,通過巖心和測井資料的綜閤分析,對新疆準東煤田西黑山勘查區西山窯組進行瞭層序地層研究,識彆齣3箇體繫域-)-低位、湖擴和高位體繫域,併進一步進行瞭高頻層序單元的劃分。在層序地層格架的約束下,分析瞭西山窯組沉積體繫的配置關繫,識彆齣辮狀河三角洲和湖泊沉積體繫,進而細分為4箇亞相和8箇微相類型。同時,對煤巖樣品進行瞭煤質分析和顯微組分定量統計,確定瞭研究區煤相類型主要為潮濕森林沼澤相和榦燥森林沼澤相。該區煤相的垂嚮縯化規律受湖平麵升降變化所控製,而湖平麵的升降受層序地層格架的約束,在不同體繫域中湖平麵的變化控製泥炭沼澤的髮育,從而決定瞭煤質煤相的縯化規律。
운용층서지층원리,통과암심화측정자료적종합분석,대신강준동매전서흑산감사구서산요조진행료층서지층연구,식별출3개체계역-)-저위、호확화고위체계역,병진일보진행료고빈층서단원적화분。재층서지층격가적약속하,분석료서산요조침적체계적배치관계,식별출변상하삼각주화호박침적체계,진이세분위4개아상화8개미상류형。동시,대매암양품진행료매질분석화현미조분정량통계,학정료연구구매상류형주요위조습삼림소택상화간조삼림소택상。해구매상적수향연화규률수호평면승강변화소공제,이호평면적승강수층서지층격가적약속,재불동체계역중호평면적변화공제니탄소택적발육,종이결정료매질매상적연화규률。
Based on the principle of sequence stratigraphy, the stratigraphic division of Xishanyao Formation in Xiheishan area is studied through the comprehensive analysis of the bore core and well logging data. As a result, such three system tracts as low-stand system tract, lake expanding system tract and high-stand system tract are recognized. Meanwhile, more para-stratigraphic sets are identified in each system tract. Therefore, braided river delta and lake depositional systems of Xishanyao Formation are deciphered into four subfacies and 8 microfacies under the constraint of sequence stratigraphic framework. Besides, coal quality and quantitative statistics of maceral are introduced in this study in order to identify the coal facies as moist forest swamp and dry forest swamp. The coal facies evolution law is controlled by the variation of lake level which was constrained under the frame-work of sequence stratigraphy in this area. As a main factor, the lake level determines the development of peat swamp, and then the evolution law of coal facies.