Genetic Analysis of the Lenticular Sand in the Paleogene Dainan Formation in Huangjue-Majiazui Area in Gaoyou Sag

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  •  The Geology Research Institute Jiangsu Oilfield,SINOPEC,Yangzhou 225012,China

Received date: 2014-03-26

  Revised date: 2014-07-13

  Online published: 2015-02-10

Abstract

Fan-delta was developed in the Dainan Formation of Gaoyou Sag,and the distribution of the sandbody was controlled by the distributary channel,but the existence of many lenticular oil-sand is inconsistent with the distribution of reservoir,so we do the genetic research on the lenticular sand.The overlapping oil-bearing area of Dainan Formation is continuous,but the oil-bearing area of the single sublayer is lenticular or allantoid.By the analysis of the water injection response,the communication of the sand is bad,response wells are little,the better response wells followed the provenance direction,but the distance of the response well is short,so the characteristic of the water injection showed that the reservoirs of the work area are with higher anisotropy.After the observation of well core,there are many soft sediment deformations,and on the base of the foreign experience,especially the theory of detrital liquid by Shanmugam,the small-size olistostrome genetic model of lithologic hydrocarbon reservoir was set up,and we think that the lenticular oil-sand was formed by the olistostrome in the layer,and the soft sediment deformation caused the bad physical property of the reservoir,so the distribution of the oil sand became lenticular.

Cite this article

LIU Jin-hua,WU Li-feng,WU Yan-mei,LIU Jian,LUO Hong-fei . Genetic Analysis of the Lenticular Sand in the Paleogene Dainan Formation in Huangjue-Majiazui Area in Gaoyou Sag[J]. Natural Gas Geoscience, 2015 , 26(2) : 261 -268 . DOI: 10.11764/j.issn.1672-1926.2015.02.0261

References

[1]Ji Youliang,Wang Yong,Li Qingshan,et al.Sediments provenance of Gaoyou Depression during sedimentation of first member of Dainan Frormation of Paleogene[J].Journal of Tongji University:Natural Science,2012,40(9):1406-1413.[纪友亮,王勇,李清山,等.高邮凹陷古近系戴南组戴一段物源分析[J].同济大学学报:自然科学版,2012,40(9):1406-1413.]
[2]Yi Wei,Wang Weifeng,Xin Ye.Study on the sedimentary evolution of Dainan Formation in south of the deep sag area in Gaoyou Sag[J].Complex Hydrocarbon Reservoirs,2010,3(2):13-16.[伊伟,王伟锋,辛也.高邮凹陷深凹带南部戴南组沉积演化研究[J].复杂油气藏,2010,3(2):13-16.]
[3]Zhou Jian,Lin Chunming,Zhang Xia,et al.Provenance system and sedimentary facies of the member 1 of Paleogene Dainan Formation in Gaoyou Sag,Jiangsu Province[J].Journal of Palaeogeography,2011,13(2):161-174.[周健,林春明,张霞,等.江苏高邮凹陷古近系戴南组一段物源体系和沉积相[J].古地理学报,2011,13(2):161-174.]
[4]Yao Yulai,Lin Chunmin,Gao Likun,et al.Sedimentary facies and evolution of the second member of the Palaeogene Dainan Formation in the deep area of eastern Gaoyou Sag Subei Basin[J].Sedimentary Geology and Tethyan Geology,2010,30(2):781-794.[姚玉来,林春明,高丽坤,等.苏北盆地高邮凹陷深凹带东部古近系戴南组二段沉积相及沉积演化[J].沉积与特提斯地质,2010,30(2):781-794.]
[5]Gao Likun,Lin Chunmin,Yao Yulai,et al.Sedimentary facies and evolution of Paleogene Dainan Formation in Gaoyou Sag,Subei Basin[J].Acta Sedimentologica Sinica,2010,28(4):706-716.[高丽坤,林春明,姚玉来.苏北盆地高邮凹陷古近系戴南组沉积相及沉积演化[J].沉积学报,2010,28(4):706-716.]
[6]Zhou Jian,Lin Chunming,Zhang Yongshan,et al.Provenance and sedimentary facies of the Dainan Formation in the Lianmengzhuang region,Gaoyou Depression,northern Jiangsu[J].Sedimentary Geology and Tethyan Geology,2012,32(2):1-9.[周健,林春明,张永山,等.苏北盆地高邮凹陷联盟庄地区戴南组物源及沉积相研究[J].沉积与特提斯地质,2012,32(2):1-9.]
[7]Shi Xiaorong,Zeng Yulan,Ma Wenrui,et al.Main controlling factors of reservoir physical porosity in Eogene Dainan Formation of HJ Oilfield in Suhei Basin[J].Journal of Oil and Gas Technology,2012,34(10):28-32.[施小荣,曾玉兰,马文睿,等.苏北盆地HJ油田古近系戴南组储层物性影响因素分析[J].石油天然气学报,2012,34(10):28-32.]
[8]Wang Yanzhong,Cao Yingchang,Li Yongxin,et al.Controlling factors on the Paleogene deep effective reservoirs in the Bonan Sag[J].Natural Gas Geoscience,2012,23(6):996-1003.[王艳忠,操应长,李永新,等.渤南洼陷古近系深层有效储层控制因素研究[J].天然气地球科学,2012,23(6):996-1003.]
[9]Lu Zhiyong.Sedimentary characteristics and model of gravity flows in Yan 18 area of the steep slope in Dongying Sag of Jiyang Depression[J].Natural Gas Geoscience,2012,23(3):420-42.[路智勇.济阳坳陷东营凹陷陡坡带盐18地区重力流沉积特征与沉积模式[J].天然气地球科学,2012,23(3):420-429.]
[10]Zheng Rongcai,Li Yun,Dai Chaocheng,et al.Depositional features of sandy debris flow of submarine fan in Zhujiang Formation,Baiyun Sag[J].Journal of Jilin University:Earth Science Edition,2012,42(6):1581-1589.[郑荣才,李云,戴朝成,等.白云凹陷珠江组深水扇砂质碎屑流沉积学特征[J].吉林大学学报:地球科学版,2012,42(6):1581-1589.]
[11]Wu Zhixiong,Yang Zhaochen,Ding Chao,et al.Characteristics of fan delta in Triassic Karamay Formation,northwest margin of Junggar Basin:Taking W16 well area as an example[J].Natural Gas Geoscience,2011,22(4):602-609.[吴志雄,杨兆臣,丁超,等.准噶尔盆地西北缘三叠系克拉玛依组扇三角洲沉积微相特征——以W16井区为例[J].天然气地球科学,2011,22(4):602-609.]
[12]Li Yun,Zheng Rongcai,Zhu Jinguo,et al.Reviews on sediment gravity flow[J].Advances in Earth Science,2011,26(2):157-165.[李云,郑荣才,朱国金,等.沉积物重力流研究进展综述[J].地球科学进展,2011,26(2):157-165.]
[13]Chen Fei,Hu Guangyi,Sun Lichun,et al.Sedimentary characteristics and the significance of petroleum exploration of sandy debris flows of Yanchang Formation of the Upper Triassin,Fuxian area,Ordos Basin[J].Acta Sedimentologica Sinica,2012,30(6):1042-1051.[陈飞,胡光义,孙立春,等.鄂尔多斯盆地富县地区上三叠统延长组砂质碎屑流沉积特征及其油气勘探意义[J].沉积学报,2012,30(6):1042-1051.]
[14]Shanmugam G,Moiola R J.Reinterpretation of depositional processes in a classic flysch sequence(Pennsylvanian Jackfork Group),Ouachita Mountains,Arkansas and Oklahoma[J].AAPG Bulletin,1995,79(5):672-695.
[15]Shanmugam G.50 years of the turbidite paradigm(1950s-1990s)deepwater processes and facies models:A critical perspective[J].Marine and Petroleum Geology,2000,17(2):285-342.
[16]Zou Caineng,Zhao Zhengzhang,Yang Hua,et al.Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J].Acta Sedimentologica Sinica,2009,12(6):1065-1075.[邹才能,赵政璋,杨华,等.陆相湖盆深水砂质碎屑流成因机制与分布特征——以鄂尔多斯盆地为例[J].沉积学报,2009,12(6):1065-1075.]
[17]Qiao Xiufu.Study of seismites of China and its prospects[J].Geological Review,1996,42(4):317-320.[乔秀夫.中国震积岩的研究与展望[J].地质论评,1996,42(4):317-320.]
[18]Yang Ping,Du Yuansheng,Xu Yajun.Eogene seismite of Huanghua Depression[J].Atca Geologica Sinica,2006,80(11):171-1715.[杨萍,杜远生,徐亚军.黄骅坳陷古近纪地震事件沉积研究[J].地质学报,2006,80(11):171-1715.]

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