珠江口盆地惠州凹陷古近系珠海组近海潮汐沉积特征
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摘要
前人研究成果多认为惠州凹陷西南部珠海组形成于辫状三角洲环境,或以受海侵影响的三角洲前缘沉积作用为主。在对研究区宏观构造—古地理背景分析之上,以岩心详细观察与描述为基础,通过岩相、测井相并辅助宏观地震相分析,提出珠海组沉积时期来自古珠江三角洲体系提供的丰富砂质沉积物在该区经历了潮汐的强烈改造作用,以潮汐沉积作用为主的认识。详细描述了发育在珠海组的潮汐沉积构造、潮下带、潮间带与潮上带沉积序列及其相组合特征,并以单井相分析为基础,结合区域地震相分析了研究区沉积相宏观展布特征。这一新认识为该区油气勘探,特别是位于该区主体部位的油气田开发中储层预测提供了依据和新思路。
Previous studies consider that Zhuhai Formation in southwestern Huizhou depression was formed in the braided delta environment,or dominated by delta front which experienced transgressive reworking.Based on the palaeogeographic background analysis,the detailed observation and description of cores,combined with the analysis of lithofacies,electro-facies and seismic facies,this study reveals that deposit of Zhuhai Formation rich-in sand supplied by the Pearl River delta experienced reworking of strong tides,and is dominated by tidal sedimentation.In this paper,tidal sedimentary structure,sedimentary sequence and facies succession of inter-tidal and supratidal facies have been detailly described.The regional distribution of depositional system in the study area has been revealed based on facies analysis of single well,combined with regional seismic facies analysis.This new understanding will be favorable for oil and gas exploration and development in this area.
Previous studies consider that Zhuhai Formation in southwestern Huizhou depression was formed in the braided delta environment,or dominated by delta front which experienced transgressive reworking.Based on the palaeogeographic background analysis,the detailed observation and description of cores,combined with the analysis of lithofacies,electro-facies and seismic facies,this study reveals that deposit of Zhuhai Formation rich-in sand supplied by the Pearl River delta experienced reworking of strong tides,and is dominated by tidal sedimentation.In this paper,tidal sedimentary structure,sedimentary sequence and facies succession of inter-tidal and supratidal facies have been detailly described.The regional distribution of depositional system in the study area has been revealed based on facies analysis of single well,combined with regional seismic facies analysis.This new understanding will be favorable for oil and gas exploration and development in this area.
引文
[1]陈长民,施和生,许世策,等.珠江口盆地(东部)第三系油气藏形成条件[M].北京:科学出版社,2003.
[2]刘昭蜀.南海地质构造与油气资源[J].第四纪研究,2000,20(1):69-76.
[3]施和生,李文湘,邹晓萍.层序地层学在珠江口盆地(东部)油田开发中的应用[J].中国海上油气(地质),2000,14(1):15-20.
[4]邓宏文,王红亮,祝永军.高分辨率层序地层学——原理及应用[M].北京:地质出版社,2002.
[5]赖内克HE,辛格I B.陆源碎屑沉积环境[M].陈昌明,李继亮,译.北京:石油工业出版社,1982.
[6]里丁HG.沉积环境与相[M].周明鉴,译.北京:科学出版社,1985.
[7]赵澄林,朱筱敏.沉积岩石学[M].3版.北京:石油工业出版社,2001.
[8]赵霞飞,吕宗刚,张闻林,等.四川盆地安岳地区须家河组——近海潮汐沉积[J].天然气工业,2008,28(4):16-18.
[9]郭英海,刘焕杰.陕甘宁地区晚古生代沉积体系[J].古地理学报,2000,2(1):19-30.
[10]Hugues Fenies,Amaury De Resseguier,Jean-Pierre Tastet.Inter-tidal clay-drape couplets(Gironde estuary,France)[J].Sedi-mentology,1999,46:1-15.
[2]刘昭蜀.南海地质构造与油气资源[J].第四纪研究,2000,20(1):69-76.
[3]施和生,李文湘,邹晓萍.层序地层学在珠江口盆地(东部)油田开发中的应用[J].中国海上油气(地质),2000,14(1):15-20.
[4]邓宏文,王红亮,祝永军.高分辨率层序地层学——原理及应用[M].北京:地质出版社,2002.
[5]赖内克HE,辛格I B.陆源碎屑沉积环境[M].陈昌明,李继亮,译.北京:石油工业出版社,1982.
[6]里丁HG.沉积环境与相[M].周明鉴,译.北京:科学出版社,1985.
[7]赵澄林,朱筱敏.沉积岩石学[M].3版.北京:石油工业出版社,2001.
[8]赵霞飞,吕宗刚,张闻林,等.四川盆地安岳地区须家河组——近海潮汐沉积[J].天然气工业,2008,28(4):16-18.
[9]郭英海,刘焕杰.陕甘宁地区晚古生代沉积体系[J].古地理学报,2000,2(1):19-30.
[10]Hugues Fenies,Amaury De Resseguier,Jean-Pierre Tastet.Inter-tidal clay-drape couplets(Gironde estuary,France)[J].Sedi-mentology,1999,46:1-15.
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