Natural Gas Geoscience

Previous Articles     Next Articles

Study on delta-deepwater fan sedimentary system of Sanya Formationin the Baodao-Changchang Depression,Qiongdongnan Basin

Yan Ying-kai,Han Yin-xue,Ma Ming,Chen Guo-jun,Lü Cheng-fu,Yang Hai-zhang,Chen Ying   

  1. 1.Key Laboratory of Petroleum Resources,Gansu Province/ Key Laboratory of Petroleum Resources Research,
    Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000,China;
    2.University of Chinese Academy of Sciences,Beijing 100049,China;
    3.CNOOC Research Institute,Beijing 100028,China
  • Received:2017-04-19 Revised:2017-08-11 Online:2017-10-10 Published:2017-10-10

Abstract:

Based on the 2D/3D seismic data,logging data and previous achievements,this paper identifies the evolutions and distributions of the Lower Miocene delta and deepwater-fan depositional system of Sanya Formation in Baodao-Changchang Depression,and analyzes the provenance characteristics and controlling factors of the sedimentary system development.The results show that there are two delta-deepwater-fan sedimentary systems of Sanya Formation in Baodao-Changchang Depression,and a large deepwater-fan developed in the center of the depression;the north slope delta of Baodao Depression,which is narrow in southwest and wide in northeast,is about 6 000km,with a distribution direction of nearly NW-SE.The north slope delta of Changchang Depression is 2 900km2 with a distribution direction of nearly N-S,the sediments of the delta are mainly derived from Hainan Island.The deepwater-fan developed both in the two delta fronts,and the distribution directions are similar to that of the upstream delta.In the center of the Baodao-Changchang Depression,large deepwater-fan with a shape of "spindle" developed,with a distribution direction of E-W and an area of 1 760km2.The main controlling factors affecting the sedimentary evolution of the delta-deepwater-fan sedimentary system are the tectonic movement,the paleo geomorphology,the source supply and so on.The discovery of the delta-deepwater-fan depositional system could provide a basis for deepwater oil-gas exploration in the Baodao-Changchang Depression.
 
 

Key words: Baodao-Changchang Depression, Sanya Formation, Delta, Deepwater-fan, Sedimentary evolution

CLC Number: 

  • TE122
[1]Zhang Gongcheng,Mi Lijun,Qu Hongjun,et al.A basic distributional framework of global deepwater basins and hydrocarbon characteristics[J].Acta petroleum Sinica,2011,32(3):369-378.[张功成,米立军,屈红军,等.全球深水盆地群分布格局与油气特征[J].石油学报,2011,32(3):369-378.]
[2]Pettingill H S. Giant field discoveries of the 1990s[J].Leading Edge,2012,20(7):698.
[3]Pettingill H S,Weimer P.Worldwide deepwater exploration and production: Past, present, and future[J].Leading Edge,2012,21(4):371.
[4]Shi Hesheng,Liu Baojun,Yan Chengzhi,et al.Hydrocarbon accumulation conditions and exploration potential in Baiyun-Liwan deepwater area, Pearl River Month Basin[J].China offshore oil and gas,2010,22(6):369-374.[施和生,柳保军,颜承志,等.珠江口盆地白云—荔湾深水区油气成藏条件与勘探潜力[J].中国海上油气,2010,22(6):369-374.]
[5]Wang Zhenfeng,Sun Zhipeng,Zhang Yingzhao,et al.Distribution and hydrocarbon accumulation mechanism of the giant deepwater Central Canyon Gasfield in Qiongdongnan Basin, northern South China Sea[J].Chinese Oil Exploration,2016,21(4):54-64.[王振峰,孙志鹏,张迎朝,等.南海北部琼东南盆地深水中央峡谷大气田分布与成藏规律[J].中国石油勘探,2016,21(4):54-64.]
[6]Xie Yuhong,Fan Caiwei,Zhou Jiaxiong,et al.Sedimentary features and controlling factors of the gravity flows in submarine fan of Middle Miocene in the Qiongdongnan Basin[J].Natural Gas Geoscience,2016,27(2):220-228.[谢玉洪,范彩伟,周家雄,等.琼东南盆地中中新世重力流海底扇沉积特征及控制因素[J].天然气地球科学,2016,27(2):220-228.]
[7]Liu Zhenghua,Chen Honghan.Hydrocarbon charging orders and times in the eastern area of Qiongdongnan Basin[J].Modern Geology,2011,25(2):279-288.[刘正华,陈红汉.琼东南盆地东部地区油气形成期次和时期[J].现代地质,2011,25(2):279-288.]
[8]Zhang Xinshun,Huang Zhilong,Fan Caiwei,et al.Fault sealing capacity and relationship with oli-gas accumulation at Baodao Northern Slope[J].Natural Gas Geoscience,2013,24(2):356-364.[张新顺,黄志龙,范彩伟,等.琼东南盆地宝岛北坡断层封闭性与油气运聚关系[J].天然气地球科学,2013,24(2):356-364.]
[9]Zhu Weilin,Mi Lijun.Atlas of Oil and Gas Basins,China Sea[M].Beijing:Petroleum Industry Press,2010.[朱伟林,米立军.中国海域含油气盆地图集[M].北京:石油工业出版社,2010.]
[10]Lei Chao,Ren Jianye,Pei Jianxiang,et al.Tectonic framework and multiple episode tectonic evolution in deepwater area of Qiongdongnan Basin,northern continental margin of South China See[J].Earth Science:Journal of China University of Geosciences,2011,36(1):151-162.[雷超,任建业,裴健翔,等.琼东南盆地深水区构造格局和幕式演化过程[J].地球科学:中国地质大学学报,2011,36(1):151-162.]
[11]Zhang Gongcheng.Tectonic evolution of deepwater area of northern continental margin in South China Sea[J].Acta petrolei  Sinica,2010,31(4):528-533.[张功成.南海北部陆坡深水区构造演化及其特征[J].石油学报,2010,31(4):528-533.]
[12]Du Tongjun.Sequence Stratigraphic and Deep Water Sedimentary Characteristic in the Qiongdongnan Basin[D].Qingdao:Ocean University of China,2013.[杜同军.琼东南盆地层序地层和深水区沉积充填特征[D].青岛:中国海洋大学,2013.]
[13]Shao Lei,Li Ang,Wu Guoxuan,et al.Evolution of sedimentary environment and provenance in Qiongdongnan Basin in the northern South China Sea[J].Acta Petroleum Sinica,2010,31(4):548-552.[邵磊,李昂,吴国瑄,等.琼东南盆地沉积环境及物源演变特征[J].石油学报,2010,31(4):548-552.]
[14]Zhong Zehong,Liu Jinghuan,Zhang Daojun,et al.Origin and sedimentary reservoir characteristics of a large submarine fan in Dongfang area,Yinggehai Basin[J].Acta Petrolei Sinica,2013,34(supplement 2):102-111.[钟泽红,刘景环,张道军,等.莺歌海盆地东方区大型海底扇成因及沉积储层特征[J].石油学报,2013,34(增刊2):102-111.]
[15]Wang Yongfeng,Wang Yingmin,Li Dong,et al.Features and source analysis on Early Pliocene sedimentary rare earth element(REE)in Central Canyon of Qiongdongnan Basin[J].Journal of Petroleum and Natural Gas,2011,33(6):50-52,68.[王永凤,王英民,李冬,等.琼东南盆地中央峡谷早上新世沉积物稀土元素特征及物源分析[J].石油天然气学报,2011,33(6):50-52,68.]
[16]Wang Ce,Liang Xinquan,Zhou Yun,et al.Construction of age frequencies of provenances on the eastern side of the Yinggehai Basin:Studies of LA-ICP-MS U-Pb ages of detrital zircons form six modern rivers,western Hainan,China[J].Earth Science Frontiers,2015,22(4):277-289.[王策,梁新权,周云,等.莺歌海盆地东侧物源年龄标志的建立:来自琼西6条主要河流碎屑锆石LA-ICP-MS U-Pb年龄的研究[J].地学前缘,2015,22(4):277-289.]
[17]Clift P D,Giosan L,Blusztajn J,et al.Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon[J].Geology,2008,36(1):79-82.
[18]Zuo Qianmei,Zhang Daojun,He Weijun,et al.Provenance analysis of Huangliu Formation of the Central Canyon system in the deepwater area of the Qiongdongnan Basin[J].Journal of Oceanography,2015,37(5):15-23.[左倩媚,张道军,何卫军,等.琼东南盆地深水区中央峡谷黄流组物源特征[J].海洋学报,2015,37(5):15-23.]
[19]Cao Licheng,Jiang Tao,Wang Zhenfeng,et al.Characteristics of heavy minerals and their implications for Neogene provenances evolution in Qiongdongnan Basin[J].Journal of Central South University:Natural Science Edition,2013,44(5):1971-1981.[曹立成,姜涛,王振峰,等.琼东南盆地新近系重矿物分布特征及其物源指示意义[J].中南大学学报:自然科学版,2013,44(5):1971-1981.]
[20]Liu Xiaofeng.The Evolution of Sedimentary Paleoenvironment and Provenance in the Deepwater Area of the Qiongdongnan Basin[D].Qingdao:Ocean University of China,2015.[刘晓锋.琼东南盆地深水区沉积古环境和物源演化[D].青岛:中国海洋大学,2015.]
[21]Cao Licheng.Provenance Evolution since Neogene in the Yinggehai and Qiongdongnan Basins:Evidence from REE,Heavy Mineral and Zircon U-Pb Ages[D].Wuhan:China University of Geosciences,2014.[曹立成.莺歌海—琼东南盆地区新近纪物源演化研究[D].武汉:中国地质大学,2014.]
[22]Yuan Yusong,Yang Shuchun,Hu Shengbiao,et al.Tectonic subsidence of Qiongdongnan Basin and its main control factors[J].Chinese Journal of Geophysics,2008,51(2):376-383.[袁玉松,杨树春,胡圣标,等.琼东南盆地构造沉降史及其主控因素[J].地球物理学报,2008,51(2):376-383.]
[23]Ji Mo,Zhang Gongcheng,Yang Haichang,et al.Structural pattern and evolution of eastern sag belt,in Deep-water area of Qiongdongnan Basin[J].Marine Geology Frontier,2014,30(9):26-35.[纪沫,张功成,杨海长,等.琼东南盆地深水区东区凹陷带结构构造及其演化特征[J].海洋地质前沿,2014,30(9):26-35.]

[1] . Feixianguan Formation lithofacies zoning and its geological significanceof eastern side of Kaijiang-Liangping Trough,NE Sichuan Basin [J]. Natural Gas Geoscience, 2018, 29(8): 1067-1077.
[2] Jia Zhi-bin,Hou Du-jie,Sun De-qiang,Jiang Yu-han,Zhang Zi-ming,Hong Mei. Geochemical characteristics of source rocks in the Lower CambrianNiutitang Formation,Guizhou Province [J]. Natural Gas Geoscience, 2018, 29(7): 1031-1041.
[3] Cao Ying-hui,Li Hong-hui,Yan Lei,Wang Hong-jiang,Zhang Jun-long,Yang Min,Zhao Yi-min. The sectional evolution characteristics of Cambrian platform margin in Manxi area ofTarim Basin and its differences in source-reservoir-cap combination conditions [J]. Natural Gas Geoscience, 2018, 29(6): 796-806.
[4] Jin Li-na,Yu Xing-he,Dong Yi-si,Shan Xin,He Yu-lin,Lin Lin. The evolution of Quaternary depositional system in gas hydrate exploration area in Qiongdongnan Basin and its relationship with BSR [J]. Natural Gas Geoscience, 2018, 29(5): 644-654.
[5] Zhang Guang-quan,Hu Xiang-yang,Sun Bing,Jia Yue-wei. Sedimentary characteristics and controlling factors of gas condensate reservoir of Ying Ⅳ formation in Longfengshan Gasfield,Songliao Basin,China [J]. Natural Gas Geoscience, 2017, 28(4): 502-513.
[6] Qian Kai,Sun Xiao-hui,Xu Xiao-qiong,Han Rong-hua,Fan Yun,Wei Xing,Chang Xin-ling,Ren Zhu-lin,Cui Ya-ya. Petroleum geology,hydrocarbon distribution and accumulation fairway study in the Lower Indus Basin [J]. Natural Gas Geoscience, 2017, 28(12): 1797-1809.
[7] Wang Zhen-sheng,Chen Chang-wei,Han Guo-meng,Ma Jian-ying,Zhou Su-yan,Hu Jin-nan,Wang Chang-li,Wang Guan-qun. Rotate-tilt slope zone structures-sedimentary evolution and petroleum geologic significance:A case study of Banqiao Slope of Qikou Sag,Bohai Bay Basin [J]. Natural Gas Geoscience, 2017, 28(11): 1650-1656.
[8] Li Ya-long,Yu Xing-he,Shan Xin,Yao Zong-quan,Li Shun-li,Sun Le,Yang Zhi-hao,Jin Li-na. The characteristics and model of the braided-river delta of the Wulabo Formation of the Sigonghe section in the southern Junggar Basin [J]. Natural Gas Geoscience, 2017, 28(11): 1678-1688.
[9] Guo Shuai,Chen Ying,Zeng Qing-bo,Yang Hai-zhang,Han Yin-xue,Ji Mo,Shen Huai-lei,Guo Jia,Zhao Zhao. Provenance evolution of delta and the effects on reservoir quality in sandstones of theupper Enping Formation in the north of Baiyun Sag,Pearl River Mouth Basin [J]. Natural Gas Geoscience, 2017, 28(10): 1527-1536.
[10] Zhang Yang,Qiu Long-wei,Yang Bao-liang,Wang Jun,Li Ji,Tian Mei-rong,Sui Shu-ling. Research on sedimentary characteristics of river dominated delta mouth bar and influences affected by water level fluctuations during the formation [J]. Natural Gas Geoscience, 2016, 27(5): 809-819.
[11] Ablimit·Imin,Tang Yong,Cao Jian,Chen Gangqiang,Chen Jing,Tao Keyu. Accumulation mechanism and enrichment rules of the continuous hydrocarbon plays in the Lower Triassic Baikouquan Formation of the Mahu Sag,Junggar Basin [J]. Natural Gas Geoscience, 2016, 27(2): 241-250.
[12] Xu Juan-juan,Jiang You-lu,Zhu Jian-feng. The application of ΔLogR technology based on the error analysis for source rock evaluation in Longfengshan Sag,Changling Faulted Depression [J]. Natural Gas Geoscience, 2016, 27(10): 1869-1877.
[13] LI Shu-tong,YAO Yi-tong,LIU Zhi-wei,WANG Yang,MOU Wei-wei,YAN Can-can. Comparative Study of Underwater Distributary Channel Sandbodiesin the Shallow-water Delta from Chang 81 of Jiyuan and Northern Shaanxi Area [J]. Natural Gas Geoscience, 2015, 26(5): 813-822.
[14] ZHU Yong-jin,YIN Tai-ju,SHEN An-jiang,LIU Ling-li,LIU Zhong-bao. Experiments on Shallow-Lacustrine Deltaic Sandstone in the Ordos Basin(Upper Paleozoic),Central China [J]. Natural Gas Geoscience, 2015, 26(5): 833-844.
[15] CHEN Ke-tong,LU Xue-song,LIU Hua,TIAN Hua,WANG Xi-han,ZHANG Bao-shou,ZHANG Ke. TOC Calculation and the Screening of Favorable Layers in the Marine Mud Shale in the Tarim Basin [J]. Natural Gas Geoscience, 2015, 26(5): 942-950.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] LI Guang-zhi, HU Bin, DENG Tian-long,YUAN Zi-yan . Petroleum Geological Significance of Microelements V and Ni[J]. Natural Gas Geoscience, 2008, 19(1): 13 -17 .
[2] MA Wen-hong, ;HE Jia-xiong ;YAO Yong-jian ;LIU Hai-ling ;WAN Zhi-feng . Characteristics of Tertiary Sediments and Main Source Rocks, Northern South China Sea[J]. Natural Gas Geoscience, 2008, 19(1): 41 -48 .
[3] XIE Wu-ren,LI Xi-zhe,ZHANG Man-lang,YANG Wei,YANG Xiao,CHENG Di . Reservoir Evaluation of Upper Triassic Xujiahe Formation in Southwest Sichuan Basin[J]. Natural Gas Geoscience, 2008, 19(1): 94 -99 .
[4] . RESEARCHES ON CHARACTERISTICS OF GEOCHEMISTRY AND FORMATIONOF WENGU 2 WELL NATURAL GAS IN DONGPU DEPRESSION[J]. Natural Gas Geoscience, 2005, 16(5): 608 -611 .
[5] . EARLY CAMBRIAN REEFS AND BANKS DEVELOPMENT IN SOUTHERNMARGIN OF DABA Mt. AND Micang Mt.[J]. Natural Gas Geoscience, 2005, 16(6): 710 -714 .
[6] CUI Sha-sha, HE Jia-xiong, CHEN Sheng-hong, Zou He-ping, CUI Jie. Development Characteristics of Pearl River Mouth Basin and  Its Geological Conditions for Oil and Gas Accumulation[J]. Natural Gas Geoscience, 2009, 20(3): 384 -391 .
[7] WANG Chi-Chao, MI Jing-Kui, LI Xian-Qiang, JIA Bao-Liang, LI Hua-Zhuan. Current Situation and Problems of Simulation  Experiment Approach of Hydrocarbon Generation[J]. Natural Gas Geoscience, 2009, 20(4): 592 -597 .
[8] Xu Wen-shi,Liu Xiu-lian,Yu Zhi-qing,Wang Jian,Gao Bin,Chai Hui. Geological Structure of Amu Darya Basin in Central Asia[J]. Natural Gas Geoscience, 2009, 20(5): 744 -748 .
[9] WANG Hai-hua,ZHANG Jun-feng,XU Hao,TANG Da-zhen. Characteristics of Fluid Inclusions and Their Application toDetermining the Times and Stages of Carboniferous VolcanicHydrocarbon Reservoirs in Malang Sag, Santanghu Basin[J]. Natural Gas Geoscience, 2009, 20(6): 890 -895 .
[10] HEJia-Xiong,WuWen-Hai, ZHUYou-Hai, CHEN Sheng-Hong, CUI Sha-Sha, GONG Xiao-Feng. Genetic Types,Migration and Accumulation of Oil & Gas and  Exploration Proposal in North Marginal Basins, South China Sea[J]. Natural Gas Geoscience, 2010, 21(1): 7 -17 .