中国石油大学学报(自然科学版)
中國石油大學學報(自然科學版)
중국석유대학학보(자연과학판)
JOURNAL OF CHINA UNIVERSITY OF PETROLEUM(EDITION OF NATURAL SCIENCE)
2015年
3期
1-7
,共7页
董春梅%马存飞%林承焰%孙雪%袁梦影
董春梅%馬存飛%林承燄%孫雪%袁夢影
동춘매%마존비%림승염%손설%원몽영
泥页岩%四组分三端元%有机质体积分数%三级命名%阜二段
泥頁巖%四組分三耑元%有機質體積分數%三級命名%阜二段
니혈암%사조분삼단원%유궤질체적분수%삼급명명%부이단
shale%four-component and three-terminal element%the volume fraction of organic matter%three-level named%the second Member of Funing Formation
泥页岩层系中成分复杂,岩相划分方案不统一。通过岩心观察、显微镜下鉴定、全岩分析及有机地化数据分析,采用岩心宏观构造、有机质含量和岩石类型相结合的方法,以“四组分三端元”分类为原则,建立一种泥页岩层系岩相综合划分方案。结果表明:该分类方案引入有机质组分的含量,体现了泥页岩层系的构造特征、混积特征及其实用性,在苏北盆地阜二段泥页岩层系岩相划分研究中得以有效应用,可以为后续泥页岩储集空间研究、测井岩相识别和储层可改造性评价奠定基础。
泥頁巖層繫中成分複雜,巖相劃分方案不統一。通過巖心觀察、顯微鏡下鑒定、全巖分析及有機地化數據分析,採用巖心宏觀構造、有機質含量和巖石類型相結閤的方法,以“四組分三耑元”分類為原則,建立一種泥頁巖層繫巖相綜閤劃分方案。結果錶明:該分類方案引入有機質組分的含量,體現瞭泥頁巖層繫的構造特徵、混積特徵及其實用性,在囌北盆地阜二段泥頁巖層繫巖相劃分研究中得以有效應用,可以為後續泥頁巖儲集空間研究、測井巖相識彆和儲層可改造性評價奠定基礎。
니혈암층계중성분복잡,암상화분방안불통일。통과암심관찰、현미경하감정、전암분석급유궤지화수거분석,채용암심굉관구조、유궤질함량화암석류형상결합적방법,이“사조분삼단원”분류위원칙,건립일충니혈암층계암상종합화분방안。결과표명:해분류방안인입유궤질조분적함량,체현료니혈암층계적구조특정、혼적특정급기실용성,재소북분지부이단니혈암층계암상화분연구중득이유효응용,가이위후속니혈암저집공간연구、측정암상식별화저층가개조성평개전정기출。
The composition of shale formation is complicated, and the lithofacies classification schemes are not unified. Using core observation, microscopic identification, whole rock analysis and organic geochemical data analysis, a comprehensive shale set lithofacies classification scheme, which is based on the principle of“four-component and three-terminal element”, was established by adopting a method of combining macro structures of cores, organic content with rock types. The classifica-tion scheme introduces the organic matter content, and reflects the structural characteristics, mixed sedimentary characteris-tics of shale formations as well as its practicability. This classification scheme has been effectively applied to the study of lithofacies classification of shale set in the second Member of Funing Formation, Subei Basin, and may form a solid basis for the future shale reservoir space research, logging lithofacies identification and reservoir reconstruction evaluation.