泌阳凹陷东南部核桃园组近岸水下扇与扇三角洲沉积特征比较及控制因素分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
南襄盆地泌阳凹陷南部陡坡带核桃园组发育大量的砂砾岩体。这些砂砾岩体与鼻状构造配置形成该凹陷重要的油气藏。但是,前人对砂砾岩体成因的研究一直存在较大的争议,主要争论集中于砂体成因是扇三角洲成因还是近岸水下扇成因。为了明确砂砾岩体的成因及平面展布,在高精度层序地层格架建立的基础上,主要利用对比的方法,从沉积相发育背景、沉积亚相及微相划分、钻测井特征、岩心特征、粒度分布特征及地震反射特征6个方面,对这两种相类型进行了总结对比,并对控制因素进行了初步的探讨。研究结果表明,边界大断裂的活动造成的断层陡缓程度的差别对工区砂体成因类型起着重要的控制作用。在平面上,断层较缓(55°~75°)的西部地区发育扇三角洲;而在断层较陡(75°~90°)的东部地区,则发育近岸水下扇。在地震剖面上,早期断层比较陡,易沉积近岸水下扇;晚期断层比较缓,易沉积扇三角洲。
Coarse-grained clastic deposits are widely developed in the Hetaoyuan Formation of the steep slope belt in southern Biyang Sag of Nanxiang Basin.They together with nose-like structures in the sag form many high-quality oil and gas reservoirs.However,the genesis of these deposits is still uncertain.The bone of contention is whether they are fan delta genesis or nearshore subaqueous fan genesis.To answer the question and get a better look at how they are distributed horizontally,we compared and summarized the two geneses and discussed their controlling factors in a stratigraphic sequence framework and from the following 6 perspectives of sedimentary settings,subfacies and microfacies categorization,drilling and logging data,core analyses,grain size distribution features and seismic response characteristics.The results show that the steepness difference of faults caused by large boundary faulting activities controlled their genesis.Horizontally,fan deltas are developed in the west area with gentle faults(55°-75°) while nearshore subaqueous fans are developed in the east area with steep faults(75°-90°) nearshore.Seismic profiles also show that early faults are steeper and favorable for the deposition of nearshore subaqueous fans; while later faults are more gentle and good for fan delta to be formed.
引文
[1]邱荣华,李纯菊.泌阳凹陷三类三角洲沉积特征及储集性能[J].石油勘探与开发,1994,21(1):99-105.Qiu Ronghua,Li Chunju.The sedimentary and reservoir characteristic of three types of deltas Biyang depression[J].Petroleum Exploration and Development,1994,21(1):99-105.
    [2]侯艳平,任建业,张青林,等.陆相裂陷盆地层序地层构成样式分析——以泌阳凹陷核三上段为例[J].地层学杂志,2005,29(1):71-76.Hou Yanping,Ren Jianye,Zhang Qinglin,et al.Analysis of the sequence stratigraphic pattern of continental rift basin—taking Biyang depression as an example[J].Journal of Stratigraphy 2005,29(1):71-76.
    [3]吕文雅,姚光庆,舒坤,等.泌阳凹陷毕店地区核三段Ⅵ-Ⅶ油组沉积微相研究[J].石油地质与工程,2014,28(4):41-45,155.Lu Wenya,Yao Guangqing,Shu Kun,et al.Sedimentary microfacies research of He-3 memberⅥ-Ⅶoil group in Bidian area of Biyang depression[J].Petroleum Geology and Engineering,2014,28(4):41-45,155.
    [4]侯贵廷,钱祥麟,蔡东升.渤海湾盆地中、新生代构造演化研究[J].北京大学学报(自然科学版),2001,37(6):845-851.Hou Guiting,Qian Xianglin,Cai Dongsheng.The tectonic evolution of Bohai Basin in Mesozoic and Cenozoic time[J].Acta Scientiarum Naturalium Universitis Pekinensis(Natural Science Edition),2001,37(6):845-851.
    [5]许胜利,朱泽栋.泌阳凹陷张扭性区域构造精细解释[J].断块油气田,2014,21(5):581-584.Xu Shengli,Zhu Zedong.Fine structural interpretation of extensional shear region in Biyang Depression[J].Fault-Block Oil and Gas Field,2014,21(5):581-584.
    [6]杨克绳.中国东部主要盆地断坳结构形成机理的探讨[J].断块油气田,1996,6(1):1-8.Yang Kesheng.Study on forming mechanism of fault sag structures in main basins in east China[J].Fault-Block Oil&Gas Field,1996,6(1):1-8.
    [7]Johnson J G,Klapper G.Devonian eustatic fluctuations in Euramerica[J].Geological Society of America Bulletin,1985,96(5):567-587.
    [8]张明安,鲜本忠.层序地层学在泌阳凹陷隐蔽油藏预测中的应用[J].石油实验地质,2003,25(4):395-402.Zhang Ming’an,Xian Benzhong.Application of sequence stratigraphy to the predicton of subtle reservoir in the Biyang depression[J].Petroleum Geology&Experiment,2003,25(4):395-402.
    [9]夏东领,李春霞,张本书.泌阳凹陷层序地层样式和油气评价[J].江汉石油学院学报,2003,25(4):36-37.Xia Donglin,Li Chunxia,Zhang Benshu.Style of sequence stratigraphy and hydrocarbon evalutiong in Biyang Depression[J].Journal of Jianghan Petroleum Institute,2003,25(4):36-37.
    [10]章新文,李吉君,朱景修,等.泌阳凹陷页岩油富集段资源评价及有利区预测[J].断块油气田,2014,21(3):301-304.Zhang Xinwen,Li Jijun,Zhu Jingxiu,et al.Resource evaluation and favorable area prediction on rich section of shale oil in Biyang Depression[J].Fault-Block Oil and Gas Field,2014,21(3):301-304.
    [11]杨傲然,贾艳雨,谭静娟,等.南阳凹陷陆相页岩油形成条件及勘探潜力分析[J].石油地质与工程,2013,27(3):8-11,145.Yang Aoran,Jia Yanyu,Tan Jingjuan,et al.Research on continental shale oil forming conditions and exploration potential analysis in Nanyang depression[J].Petroleum Geology and Engineering,2013,27(3):8-11,145.
    [12]朱筱敏.沉积岩石学[M].北京:石油工业出版社,2008:229-234.Zhu Xiaomin.Sedimentary petrology[M].Beijing:Petroleum Industry Press,2008:229-234.
    [13]鄢继华,陈世悦,姜在兴.东营凹陷北部陡坡带近岸水下扇沉积特征[J].石油大学学报(自然科学版),2005,29(1):12-21.Yan Jihua,Chen Shiyue,Jiang Zaixing.Sedimentary characteristic of nearshore subaqueous fans in steep slope of Dongying depression[J].Journal of University of Petroleum(Natural Science Edition),2005,29(1):12-21.
    [14]鲜本忠,姜在兴.河南泌阳凹陷古近系核桃园组核二段沉积体系[J].古地理学报,2002,2(4):31-37.Xian Benzhong,Jiang Zaixing.Sedimentary systems in the member 2of Hetaoyuan Formation of Paleogene in Biyang depression of Henan province[J].Journal of Palaeogeography,2002,2(4):31-37.
    [15]朱筱敏,董艳蕾,胡廷惠,等.精细层序地层格架与地震沉积学研究——以泌阳凹陷核桃园组为例[J].石油与天然气地质,2011,32(4):615-624.Zhu Xiaomin,Dong Yanlei,Hu Tinghui,et al.Seismic sedimentology study of fine sequence stratigraphic framework:a case study of the Hetaoyuan Formation in the Biyang Sag[J].Oil&Gas Geology,2011,32(4):615-624.
    [16]秦中正,秦飞,金燕林,等.王集油田沉积特征与沉积微相展布研究[J].石油地质与工程,2013,27(6):30-33.Qin Zhongzheng,Qin Fei,Jin Yanlin,et al.Study on sedimentary characteristics and sedimentary microfacies distribution of Wangji oilfield[J].Petroleum Geology and Engineering,2013,27(6):30-33.
    [17]廖纪佳,朱筱敏.南襄盆地泌阳凹陷深凹区核三段沉积特征及演化[J].地球科学报,2012,33(2):167-175.Liao Jijia,Zhu Xiaomin.Sedimentary characteristic and evolution of He-3 formation in deep area of Biyang sag,Nanxiang basin[J].Acta Geoscientica Sinica,2012,33(2):167-175.
    [18]隋风贵,操应长,刘慧民,等.东营凹陷北带东部古近系近岸水下扇储集物演化及其油气成藏模式[J].地质学报,2010,84(2):246-256.Sui Fenggui,Cao Yingchang,Liu Huimin,et al.Physical properties evolution and hydrocarbon accumulation of Paleogene nearshore subaqueous fan in the eastern north margin of the Dongying depression[J].Acta Geologica Sinica,2010,84(2):246-256.
    [19]杨树彬,庄升,李伟.欢喜岭地区沙三段大凌河油层近岸水下扇沉积特征[J].西安石油大学学报(自然科学版),2010,25(4):10-15.Yang Shubin,Zhuang Sheng,Li Wei.Sedimentary characteristic of nearshore subaqueous fan of Dalinghe reservoir of Es3in Huanxiling area[J].Journal of Xi’an Shiyou University(Natural Science Edition),2010,25(4):10-15.
    [20]赵红兵,严科.近岸水下扇砂砾岩沉积特征及扇体分布规律[J].断块油气田,2011,18(4):438-441.Zhao Hongbing,Yan Ke.Depositional characteristic of glutenite and distribution pattern of fan on nearshore subaqueous fan[J].FaultBlock Oil&Gas Field,2011,18(4):438-441.
    [21]苗长盛,刘招君,方石,等.塔南凹陷南屯组近岸水下扇沉积特征及有利含油相带分析[J].中国石油大学学报(自然科学版),2011,35(1):34-39.Miao Changsheng,Liu Zhaojun,Fang Shi,et al.Sedimentary characteristic and favorable oil-bearing facies belts analysis of nearshore subaqueous fan of Nantun formation in Tanan depression[J].Journal of China University of Petroleum(Natural Science Edition),2011,35(1):34-39.
    [22]远光辉,操应长,王艳忠.东营凹陷民丰地区沙河街组四段—三段中亚段沉积相与沉积演化特征[J].石油与天然气地质,2012,33(2):277-286.Yuan Guanghui,Cao Yingchang,Wang Yanzhong.Sedimentary facies and their evolution of the 4th-middle 3rd members of Shahejie Formation in Minfeng area,Dongying Sag[J].Oil&Gas Geology,2012,33(2):277-286.
    [23]李志明,张隽,余晓露,等.南襄盆地泌阳凹陷烃源岩成熟度厘定及其意义[J].石油实验地质,2013,35(1):76-80.Li Zhiming,Zhang Jun,Yu Xiaolu.Determination of maturity for source rocks in Biyang Sag of Nanxiang Basin and its significance[J].Petroleum Geology&Experiment,2013,35(1):76-80.
    [24]孙鸣,王华,廖远涛,等.福山凹陷白莲地区流沙港组一段扇三角洲沉积体系与油气成藏条件分析[J].中南大学学报(自然科学版),2013,44(10):4150-4160.Sun Ming,Wang Hua,Liao Yuantao,et al.Analysis on fan-delat sedimentary system and reservoir-forming conditions of the first member of Liushagang formation in Bailian area of Fushan sag[J].Journal of Central South University(Natural Science Edition),2013,44(10):4150-4160.
    [25]谭程鹏,于兴河,李胜利,等.准噶尔盆地南缘四棵树剖面八道湾组扇三角洲沉积特征[J].现代地质,2014,28(1):180-189.Tan Chengpeng,Yu Xinghe,Li Shengli,et al.Sedimentary characteristic of fan delta of the badaowan formation Sikeshu section,Southern Junggar Basin[J].Geoscience,2014,28(1):180-189.
    [26]刘宗堡,赵容生,闫力,等.海-塔盆地塔南凹陷南屯组一段沉积体系特征[J].石油与天然气地质,2013,34(6):743-750.Liu Zongbao,Zhao Rongsheng,Yan Li,et al.Depositional system characteristics of the first member of the Nantun Formation in Tanan sag,the Hai-Ta Basin[J].Oil&Gas Geology,2013,34(6):743-750.
    [27]李占东,李阳,刘云利,等.松辽盆地南部东南隆起区白垩系登娄库组沉积特征[J].石油与天然气地质,2014,35(3):401-409.Li Zhandong,Li Yang,Liu Yunli,et al.Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin[J].Oil&Gas Geology,2014,35(3):401-409.
    [28]刘家铎,田景春,何建军,等.近岸水下扇沉积微相及储层的控制因素研究——以沾化凹陷罗家鼻状构造沙四段储层为例[J].成都理工学院学报,1999,26(4):365-369.Liu Jiaduo,Tian Jingchun,He Jianjun,et al.A study of sedimentary microfacies and controlling factors of the reservoir of the nearshore subaqueous fan—Taking the fourth member of the Shahejie formation in the Luojia nose,Zhanhua depression for an example[J].Journal of Chengdu University of Technology,1999,26(4):365-369.
    [29]李祺,陈振林,汤济广.下二门油田核二段沉积微相粒度概率累积曲线[J].断块油气田,2008,15(4):24-27.Li Qi,Chen Zhenlin,Tang Jiguang.Characteristic of probability cumulative curves of granularity in sedimentary microfacies at the second member of Hetaoyuan formation[J].Fault-Block Oil&Gas Field,2008,15(4):24-27.
    [30]肖晨曦,李志忠.粒度分析及其在沉积学中应用研究[J].新疆师范大学学报(自然科学版),2006,25(3):118-123.Xiao Chenxi,Li Zhizhong.The research summary of grain size analysis and its application in the sedimentation[J].Journal of Xinjiang Normal University(Natural Science Edition),2006,25(3):118-123.
    [31]袁静,杜玉民,李云南.惠民凹陷古近系碎屑岩主要沉积环境粒度概率累积曲线特征[J].石油勘探与开发,2003,30(3):103-106.Yuan Jing,Du Yumin,Li Yunnan.Probability cumulative grain size curves in terrigenous depositional environments of the paleogene in Huimin sag[J].Petroleum Exploration and Development,2003,30(3):103-106.
    [32]袁文芳,陈世悦,曾昌民.柴达木盆地西部地区第三系碎屑岩粒度概率累积曲线特征[J].石油大学学报(自然科学版),2005,29(5):12-18.Yuan Wenfang,Chen Shiyue,Zeng Changmin.Probability cumulative grain size curves in terrigenous of the Tertiary in west Qaidam basin[J].Journal of the University of Petroleum(Natural Science Edition),2005,29(5):12-18.
    [33]刘建生,邓传伟.宁晋断裂陡坡带近岸水下扇体储层的地震预测[J].石油物探,2010,49(4):380-384.Liu Jiansheng,Deng Chuanwei.Seismic prediction of nearshore underwater fan reservoir in Ningjin fractured steep slope belt[J].Geophysical Prospecting for Petroleum,2010,49(4):380-384.
    [34]王升兰,刘晖.珠江口盆地开平凹陷恩平组地震反射特征与沉积体系展布[J].科技导报,2014,32(28/29):64-69.Wang Shenglan,Liu Hui.Seismic reflection and depositional system of the Enping formation in the Kaiping deposition of the Zhujiangkou Basin[J].Science&Technology Review,2014,32(28/29):64-69.
    [35]杨香华,孙永传,孙家振.泌阳凹陷下第三系的层序地层格架及其对边界断裂、古气候和物源的响应[J].地球科学——中国地质大学学报,1994,19(5):676-684.Yang Xianghua,Sun Yongchuan,Sun Jiazhen.Lower tertiary sequence stratigraphy framework and its’s response to boundary faults,Paleoclimate and sediment source in Biyang depression[J].Earth Science—Journal of China University of Geosciences,1994,19(5):676-684.
    [36]张明安,鲜本忠.泌阳凹陷构造活动的沉积响应[J].西安石油大学学报(自然科学版),2004,19(2):9-12.Zhang Ming’an,Xian Benzhong.Response of sedimentation to structural evolution in Biyang sag[J].Journal of Xi’an Shiyou University(Natural Science Edition),2004,19(2):9-12.

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