Wei Wei, Lu Yongchao, Liu Zhongrong, Pan Lei, Lin Weibing, Jian Hui. Sequence stratigraphic framework and sedimentary model of Niubao Formation in Lunpola Basin, central Tibet[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 32-40. doi: 10.11781/sysydz201701032
Citation: Wei Wei, Lu Yongchao, Liu Zhongrong, Pan Lei, Lin Weibing, Jian Hui. Sequence stratigraphic framework and sedimentary model of Niubao Formation in Lunpola Basin, central Tibet[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 32-40. doi: 10.11781/sysydz201701032

Sequence stratigraphic framework and sedimentary model of Niubao Formation in Lunpola Basin, central Tibet

doi: 10.11781/sysydz201701032
  • Received Date: 2016-06-06
  • Rev Recd Date: 2016-12-05
  • Publish Date: 2017-01-28
  • Based on an integrated investigation of well logging, seismic data, cores and outcrops, the Niubao Formation in the Lunpola Basin was subdivided into one first order sequence, three second order sequences, corresponding to the first, second and third members of Niubao Formation, and seven third order sequences from base to top, namely SQ1, SQ2, SQ3, SQ4, SQ5, SQ6, and SQ7. Two sequence stratigraphic patterns including faulted slope zone and flexure slope break zone were identified within the sequence stratigraphic framework. There are several exploration targets, including fan deltas on the gentle slope of HST and large-scale low stand fans in the slope break zone of LST in the flexure slope break zone, and high stand braided river deltas and large-scale low stand fans in the slope break zone in the faulted slope zone. A sedimentary model was established through the analyses of spatial and temporal distribution of the sequences. Three main sand bodies developed in the Niubao Formation, namely the northern, southwestern and eastern sand bodies, and their distribution was controlled by the slope break zone.

     

  • [1]
    杜佰伟,谭富文,陈明.西藏伦坡拉盆地沉积特征分析及油气地质分析[J].沉积与特提斯地质,2004,24(4):46-54. Du Baiwei,Tan Fuwen,Chen Ming.Sedimentary features and petroleum geology of the Lunpola Basin, Xizang[J].Sedimentary Geology and Tethyan Geology,2004,24(4):46-54.
    [2]
    顾忆,邵志兵,叶德燎,等.西藏伦坡拉盆地烃源岩特征及资源条件[J].石油实验地质,1999,21(4):340-345. Gu Yi,Shao Zhibing,Ye Deliao,et al.Characteristics of source rocks and resource prospect in the Lunpola Basin,Tibet[J].Experimental Petroleum Geology,1999,21(4):340-345.
    [3]
    雷清亮,戴国汉,傅孝悦.西藏油气远景分析[J].石油与天然气地质,1996,17(1):22-26. Lei Qingliang,Dai Guohan,Fu Xiaoyue.Analysis hydrocarbon prospects of in Tibet[J].Oil & Gas Geology,1996,17(1):22-26.
    [4]
    李宇平,范小军.断拗型盆地构造-沉积模式与隐蔽性油藏:以西藏伦坡拉盆地古近系为例[J].地质与勘探,2015,51(4):789-796. Li Yuping,Fan Xiaojun.Structure-sedimentary model and subtle reservoirs in fault-depression basins:An example of the Paleogene system in the Lunpola Basin,Tibet[J].Geology and Exploration,2015,51(4):789-796.
    [5]
    马鹏飞,王立成,冉波.青藏高原中部新生代伦坡拉盆地沉降史分析[J].岩石学报,2013,29(3):990-1002. Ma Pengfei,Wang Licheng,Ran Bo.Subsidence analysis of the Cenozoic Lunpola Basin,central Qinghai-Tibetan Plateau[J].Acta Petrologica Sinica,2013,29(3):990-1002.
    [6]
    Ma Pengfei,Wang Chengshan,Wang Licheng,et al.Sedimentology and organic properties of Lower Tertiary lacustrine source rocks,Lunpola Basin,central Tibetan Plateau:Implications for hydrocarbon potential[J].Marine and Petroleum Geology,2015,66(Part 4):1029-1041.
    [7]
    孙涛,王成善,李亚林,等.西藏中部伦坡拉盆地古近系沉积有机质特征及意义[J].地球化学,2012,41(6):530-537. Sun Tao,Wang Chengshan,Li Yalin,et al.Characteristics and signi-ficance of sedimentary organic matter in the Paleogene of Lunpola Basin, central Tibet[J].Geochimica,2012,41(6):530-537.
    [8]
    孙涛.西藏伦坡拉盆地古近系层序地层学及岩性圏闭研究.北京:中国地质大学(北京),2013. Sun Tao.Sequence stratigraphy and lithologic trap predication in the Lunpola Basin.Beijing:China University of Geoscience (Beijing),2013.
    [9]
    孙玮,李智武,肖秋苟,等.西藏伦坡拉盆地北缘中深层古近系牛堡组油气成藏分析[J].成都理工大学学报(自然科学版),2015,42(4):419-426. Sun Wei,Li Zhiwu,Xiao Qiugou,et al.Analysis of petroleum accumulation of Paleogene Niubao Formation in middle-deep underground on north margin of Lunpola Basin,Tibet,China[J].Journal of Chengdu University of Technology (Science & Technology Edition),2015,42(4):419-426.
    [10]
    Sun Tao,Wang Chengshan,Duan Yi,et al.The organic geochemistry of the Eocene-Oligocene black shales from the Lunpola Basin,central Tibet[J].Journal of Asian Earth Sciences,2014,79:468-476.
    [11]
    谢尚克,杜佰伟,王剑,等.西藏伦坡拉盆地油页岩特征及分布规律[J].吉林大学学报(地球科学版),2014,44(6):1760-1767. Xie Shangke,Du Baiwei,Wang Jian,et al.Characteristics and distribution rule of oil shale in Lunpola Basin,Tibet[J].Journal of Jilin University (Earth Science Edition),2014,44(6):1760-1767.
    [12]
    Fu Xiugen,Jian Wang,Chen Wenbin,et al.Organic accumulation in lacustrine rift basin:Constraints from mineralogical and multiple geochemical proxies[J].International Journal of Earth Sciences,2015,104(2):495-511.
    [13]
    冯有良.东营凹陷下第三系层序地层格架及盆地充填模式[J].地球科学(中国地质大学学报),1999,24(6):635-642. Feng Youliang.Lower tertiary sequence stratigraphic framework and basin filling model in Dongying Depression[J].Earth Science(Journal of China University of Geosciences),1999,24(6):635-642.
    [14]
    李相博,郭彦如,刘化清,等.浅谈小波分析在鄂尔多斯盆地延长组层序地层划分中的应用[J].天然气地球科学,2006,17(6):779-782. Li Xiangbo,Guo Yanru,Liu Huaqing,et al.The application of wavelet analysis in sequence stratigraphic subdivision of the Yanchang Formation,Ordos Basin[J].Natural Gas Geoscience,2006,17(6):779-782.
    [15]
    赵伟,姜在兴,邱隆伟,等.小波分析划分层序单元的地质学理论基础、方法与应用[J].石油与天然气地质,2010,31(4):436-441. Zhao Wei,Jiang Zaixing,Qiu Longwei,et al.Geological concept,method and application of sequence unit identification through wavelet analysis[J].Oil & Gas Geology,2010,31(4):436-441.
    [16]
    朱筱敏,康安,王贵文.陆相坳陷型和断陷型湖盆层序地层样式探讨[J].沉积学报,2003,21(2):283-287. Zhu Xiaomin,Kang An,Wang Guiwen.Sequence stratigraphic models of depression and faulted-down lake basins[J].Acta Sedimentologica Sinica,2003,21(2):283-287.
    [17]
    王华,廖远涛,陆永潮,等.中国东部新生代陆相断陷盆地层序的构成样式[J].中南大学学报(自然科学版),2010,41(1):277-285. Wang Hua,Liao Yuantao,Lu Yongchao,et al.Sequence architecture styles of Cenozoic continental rift basins in East China[J].Journal of Central South University (Science and Technology),2010,41(1):277-285.
    [18]
    任建业,陆永潮,张青林.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[J].地球科学(中国地质大学学报),2004,29(5):596-602. Ren Jianye,Lu Yongchao,Zhang Qinglin.Forming mechanism of structural slope-break and its control on sequence style in faulted basin[J].Earth Science(Journal of China University of Geosciences),2004,29(5):596-602.
    [19]
    董艳蕾,朱筱敏,李德江,等.渤海湾盆地辽东湾地区古近系地震相研究[J].沉积学报,2007,25(4):554-563. Dong Yanlei,Zhu Xiaomin,Li Dejiang,et al.Seismic facies of Paleogene in Liaodong Bay,Bohai Basin[J].Acta Sedimentologica Sinica,2007,25(4):554-563.
    [20]
    张兵,王绪本,周刚,等.大川中地区须家河组二、四段地震相与沉积相研究[J].海洋地质前沿,2013,29(3):13-21. Zhang Bing,Wang Xuben,Zhou Gang,et al.Study of seismic and sedimentary facies of the 2nd and 4th members of the Xujiahe Formation in the Great Central Sichuan[J].Marine Geology Frontiers,2013,29(3):13-21.
  • Relative Articles

  • Cited by

    Periodical cited type(9)

    1. 刘海涛,何志勇. 曲线重构技术在伦坡拉盆地储层预测中的应用. 重庆科技学院学报(自然科学版). 2022(03): 39-44 .
    2. 仇永峰,刘启东,于雯泉,李鹤永,李维. 苏北盆地隐蔽油藏勘探实践及认识. 复杂油气藏. 2021(02): 1-7 .
    3. 曾胜强,王剑,陈文彬,付修根,孙伟,李金锋,刘君豪. 伦坡拉盆地西部丁青湖组新发现凝灰岩锆石U-Pb年龄及其地层学意义. 地质学报. 2020(08): 2354-2366 .
    4. 赵帅,解习农,刘中戎,陆扬博,肖苏芸,邓雨恬. 古地貌对断陷盆地沉积体系的控制作用:以青藏高原伦坡拉盆地始新统牛堡组为例. 地质科技情报. 2019(02): 53-64 .
    5. 武群虎,郝冉冉,周红科,刘少斌,李洋. 埕岛东坡东营组高精度层序地层格架与储层预测. 特种油气藏. 2019(05): 1-7 .
    6. 郑超,王宇峰,汤兴宇,胡欣,孙志昀. 双鱼石地区栖霞组层序地层划分及沉积相分析. 特种油气藏. 2018(04): 39-45 .
    7. 郝景宇,马成宪,李旭文,潘磊,肖继林. 伦坡拉盆地牛堡组砂砾岩致密化与孔隙成因. 西南石油大学学报(自然科学版). 2018(03): 11-22 .
    8. 刘中戎,曹强,何志勇. 西藏伦坡拉盆地牛堡组一段沉积特征及勘探意义. 地质科技情报. 2017(06): 174-180 .
    9. 刘玉瑞. 苏北盆地戴南组泥屑流扇沉积. 石油与天然气地质. 2017(03): 419-429 .

    Other cited types(5)

  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-082024-092024-102024-112024-122025-012025-022025-032025-042025-052025-062025-0701020304050
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 19.0 %FULLTEXT: 19.0 %META: 79.7 %META: 79.7 %PDF: 1.4 %PDF: 1.4 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 4.4 %其他: 4.4 %Central District: 0.3 %Central District: 0.3 %China: 0.4 %China: 0.4 %Germany: 0.1 %Germany: 0.1 %India: 0.1 %India: 0.1 %三门峡: 0.3 %三门峡: 0.3 %上海: 0.3 %上海: 0.3 %不列颠哥伦比亚: 0.2 %不列颠哥伦比亚: 0.2 %临汾: 0.1 %临汾: 0.1 %北京: 2.9 %北京: 2.9 %南通: 0.1 %南通: 0.1 %嘉兴: 0.2 %嘉兴: 0.2 %天津: 0.2 %天津: 0.2 %太原: 0.1 %太原: 0.1 %宣城: 0.1 %宣城: 0.1 %山景城: 0.1 %山景城: 0.1 %常州: 0.1 %常州: 0.1 %平顶山: 0.1 %平顶山: 0.1 %张家口: 2.4 %张家口: 2.4 %惠州: 0.1 %惠州: 0.1 %扬州: 0.1 %扬州: 0.1 %新乡: 0.1 %新乡: 0.1 %无锡: 0.1 %无锡: 0.1 %晋城: 0.1 %晋城: 0.1 %杭州: 1.1 %杭州: 1.1 %柏林: 1.0 %柏林: 1.0 %武汉: 0.2 %武汉: 0.2 %汉堡: 0.1 %汉堡: 0.1 %沃思堡: 0.3 %沃思堡: 0.3 %淄博: 0.1 %淄博: 0.1 %深圳: 0.1 %深圳: 0.1 %温州: 0.3 %温州: 0.3 %湘潭: 0.1 %湘潭: 0.1 %漯河: 0.1 %漯河: 0.1 %百色: 0.2 %百色: 0.2 %盘锦: 0.1 %盘锦: 0.1 %石家庄: 0.1 %石家庄: 0.1 %芒廷维尤: 50.0 %芒廷维尤: 50.0 %芝加哥: 0.3 %芝加哥: 0.3 %莫斯科: 0.8 %莫斯科: 0.8 %西双版纳傣族自治州: 1.0 %西双版纳傣族自治州: 1.0 %西宁: 28.2 %西宁: 28.2 %西安: 0.6 %西安: 0.6 %贵阳: 0.1 %贵阳: 0.1 %运城: 0.2 %运城: 0.2 %遵义: 0.1 %遵义: 0.1 %邯郸: 0.1 %邯郸: 0.1 %郑州: 0.3 %郑州: 0.3 %长沙: 0.1 %长沙: 0.1 %长治: 0.1 %长治: 0.1 %阿什本: 0.8 %阿什本: 0.8 %香港: 0.1 %香港: 0.1 %其他Central DistrictChinaGermanyIndia三门峡上海不列颠哥伦比亚临汾北京南通嘉兴天津太原宣城山景城常州平顶山张家口惠州扬州新乡无锡晋城杭州柏林武汉汉堡沃思堡淄博深圳温州湘潭漯河百色盘锦石家庄芒廷维尤芝加哥莫斯科西双版纳傣族自治州西宁西安贵阳运城遵义邯郸郑州长沙长治阿什本香港

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (1471) PDF downloads(294) Cited by(14)
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return