断陷盆地单因素精细取证下的沉积体系综合分析——以歧口凹陷古近系沙三二亚段为例
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
在对歧口凹陷古近系沙三二亚段的多种单因素沉积学信息——测井相、岩心相、砂分散体系、地震相和地震属性、生物相、矿物岩石学和有机地化与岩石(颜色)、构造、古地貌等分别进行了详细研究的基础上,系统地对多种单因素沉积学信息的空间分布规律和空间配置关系进行了综合分析,总结了沉积学的共性和特殊性规律,使多种单因素沉积学信息起到了相互佐证和互为补充的作用,从而有效地对研究区沉积体系类型、空间配置关系和物源进行了客观的分析和评价。研究认为,歧口凹陷沙三二亚段发育4种主要的沉积体系类型:扇三角洲沉积体系、辫状河三角洲沉积体系、水下扇沉积体系和湖泊沉积体系。其中,在断层活动性强、坡度较陡的地区发育扇三角洲;在坡度较缓的地区发育辫状河三角洲;断控盆地边缘深水区发育近岸水下扇,盆地内部次级断层则控制了远岸水下扇的发育。沉积体系的空间配置受5大主要物源控制:燕山物源、沧县物源、埕宁物源、孔店物源和沙垒田物源。本研究证明,这种"单因素精细取证,多因素综合分析"的方法在拥有丰富勘探资料的断陷盆地沉积体系研究中行之有效。
Qikou sag is a typical Paleogenic fault basin in eastern China with an exploration and development history of about half a century and abundant geologic information.First,the multiple factors of the second sub-member of the third member of the Paleogenic Shahejie Formation in the Qikou sag,including logging facies,core facies,sand distributed system,seismic facies and seismic attribution,biofacies,mineralogy and petrology,organic geochemistry,rock color,structure,paleogeomorphology,were studied in detail.Then,the spatial distribution and arrangement of these factors were analyzed systematically to decipher the sedimentology.The consistent sedimentology information enable objective analysis and valuation for the depositional system types,spatial arrangement and provenances.There are four types of depositional systems in the second sub-member of the third member of the Shahejie Formation in the Qikou sag,i.e.,fan delta depositional system,braided delta depositional system,submarine fan depositional system and lacustrine depositional system.Fan delta depositional system developed in the steep area with extensive fault activity;braided delta depositional system developed in the smooth areas ;inshore submarine fan depositional system developed in the fault basin margin and infralittoral submarine fan depositional system was controlled by intrabasinal secondary faults.They were influenced by five main provenances,the Yanshan,Cangxian,Chengning,Kongdian and Shaleitian provenances.It shows that comprehensive analysis of multiple factors with details was effective for the depositional system analysis of fault basins with abundant exploration data.
引文
艾能平,任建业,祁鹏,史双双,佟殿君,胡德胜.2009.歧口凹陷伸展滑脱构造系统的厘定及其地质意义.大地构造与成矿学,33(3):343-351.
    陈昭年,陈发景,周建生,石彦民.1997.黄骅坳陷中北区和歧口凹陷断裂构造特征及古应力分析.现代地质,11(4):471-477.
    程日辉,郑和荣,林畅松.1999.构造断阶与砂体预测:以沾化凹陷富林地区为例.石油与天然气地质,20(3):203-206.
    戴俊生,漆家福,陆克政,李理.1998.渤海湾盆地早第三纪构造样式与油气藏的关系.石油大学学报(自然科学版),22(2):1-7.
    冯有良,周海民,李思田,刘蕴华,董月霞,曹中宏.2004.陆相断陷盆地层序类型与构造特征.地质论评,50(1):43-48.
    郭兴伟,施小斌,丘学林,吴智平,杨小秋,肖尚斌.2007.渤海湾盆地新生代沉降特征及其动力学机制探讨.大地构造与成矿学,31(3):273-280.
    姜华,王华,肖军,林正良,蔡佳.2009.应用古地貌分析方法进行有利区带预测——以琼东南盆地[2]号断裂带为例.石油勘探与开发,36(4):436-441.
    焦养泉,李珍,周海民.1998.沉积盆地物质来源综合研究——以南堡老第三纪亚断陷盆地为例.岩相古地理,18(5):16-20.
    赖生华,李晓宏.2007.断陷盆地沉积体系研究新思路:从古地貌、岩性变化、水体深度到沉积体系.沉积学报,25(5):663-670.
    林畅松,潘元林,肖建新,孔凡仙,刘景彦,郑和荣.2000.“构造坡折带”——断陷盆地层序分析和油气预测的重要概念.地球科学——中国地质大学学报,25(3):260265.
    蒲秀刚,吴永平,周建生,杨池银,廖前进,周立宏,肖敦清,査明,柳飒.2007.歧口凹陷岩性地层油气藏特征及勘探潜力.石油学报,28(2):35-39.
    渠芳,陈清华,连承波,张军涛,蔡福龙.2008.黄骅坳陷南区油气分布规律及其成藏机制.石油勘探与开发,35(3):294-300.
    任建业,陆永潮,张青林.2004.断陷盆地构造坡折带形成机制及其对层序发育样式的控制.地球科学——中国地质大学学报,29(5):596-602.
    王光奇,李三忠,周立宏,岳云福,高振平,单业华.2002.张东断层成因机制及其与油气关系.石油勘探与开发,29(6):38-40.
    王华,白云风,黄传炎,严德天,刘彦博,陈思,向雪梅,廖计华,夏存银,赵淑娥.2009.歧口凹陷古近纪东营期古物源体系重建与应用.地球科学——中国地质大学学报,34(3):448-456.
    王华,廖远涛,陆永潮,任建业,王家豪,严德天,刘彦博.2010.中国东部新生代陆相断陷盆地层序的构成样式.中南大学学报(自然科学版),41(1):277-285.
    吴永平,付立新,杨池银,靳久强.2002.黄骅坳陷中生代构造演化对潜山油气成藏的影响.石油学报,23(2):1621.
    徐振中,陈世悦,姚军,王永诗.2008.济阳坳陷中生代构造活动与沉积作用的时空关系.大地构造与成矿学,32(3):317-325.
    严德天,王华,肖敦清,王家豪,廖远涛.2007.黄骅坳陷中部沙三段沉积体系分析.石油勘探与开发,34(3):328334.
    Francisco S,Antonio G,Khalil E K,Carlos S G.,Angel C L,Manuel M and Rachid H.2007.Tectono-sedimentary setting of the Oligocene-early Miocene deposits on the BeticRifian internal zone(Spain and Morocco).Geobios,40(2):191-205.
    Galloway W E and Hobday D K.1983.Terrigenous clastic depositional systems—applications to petroleum,coal,and uranium exploration.Springer,New York Heidelberg,117-230.
    Hans E,Mandana H and Wolfgang S.2002.Tectonic and climatic control of Paleogene sedimentation in RhenodanubianFlysch basin(Eastern Alps,Austria).Basin Research,14(7):247-262.
    Posamentier H W and Allen G P.1999.Siliciclastic sequencestratigraphy:Concepts and applications.SEPM Concepts inSedimentology and Paleontology,7:210.
    Posamentier H W and Kolla V.2003.Seismic geomorphologyand stratigraphy of depositional elements in deep-water settings.Journal of Sedimentary Research,73(3):367388.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心