Advanced Search
Volume 33 Issue 3
. 
Turn off MathJax
Article Contents
Abstract
References
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2011  >  33(3): 274-281
ZHANG Shouchun, WANG Xuejun, WANG Xiuhong, ZHU Rifang, QIU Yibo. Dynamic difference and characterization of reservoir fluid in continental rift basins[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 941-949. doi: 10.11781/sysydz202206941
Citation: Li Rong, Zhang Di, Zhu Lixia. Densification of Upper Triassic Xujiahe tight sandstones, Western Sichuan, China[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(3): 274-281. doi: 10.11781/sysydz201103274
shu

Densification of Upper Triassic Xujiahe tight sandstones, Western Sichuan, China

doi: 10.11781/sysydz201103274

  • Chengdu Institute of Geology and Mineral Resources, Chengdu, Sichuan 610081, China

  • Received Date: 2011-01-06
  • Rev Recd Date: 2011-04-11
  • Publish Date: 2011-06-28
    Abstract
  • Densification process of the Upper Triassic Xujiahe sandstones were described based on petrologic,diagenesis and basin modeling analyses.The diagenetic events that affect reservoir quality mainly include mechanical and chemical compactions,precipitation of carbonate cements,and cementation by quartz.Compaction is the dominant process of porosity loss.Sandstones with high content of quartz,feldspar and carbonate rock fragment exhibit higher mechanical stability.Pervasive mesogenetic carbonate cementation occurs in the calcarenaceous sandstones in T3x4 and the fine-grained sandstones in T3x2 and reservoir quality is significantly deteriorated by extensive carbonate cementation.Open and paleo-high environment is favorable for relatively good reservoir quality.Quartz cements are mainly sourced by the pressure dissolution of detrital quartz and are more abundant in sandstones rich in detrital quartz and illite and poor in carbonate cements and chlorite.Thick and continuous chlorite pore-linings help to preserve porosity by inhibiting pressure dissolution and quartz cementation and thus can be doubly beneficial to the Xujiahe sandstones.

     

    • FullText(HTML)
    • References(26)
  • [1]
    杨长清,刘树根,曹波,等.龙门山造山带与川西前陆盆地耦合关系及其对油气成藏的控制[J].成都理工大学学报(自然科学版),2008,35(4):471-476.
    [2]
    李书兵,何鲤,柳梅青.四川盆地晚三叠世以来陆相盆地演化史[J].天然气工业,1999,19(增刊):18-23.
    [3]
    罗啸泉,陈兰.川西坳陷形成演化及其与油气的关系[J].油气地质与采收率,2004,11(1):16-19.
    [4]
    曾洪扬,陈洪德,林良彪,等.川西前陆盆地晚三叠世构造层序岩相古地理特征[J].石油实验地质,2009,31(1):46-49.
    [5]
    蔡希源.深层致密砂岩气藏天然气富集规律与勘探关键技术:以四川盆地川西坳陷须家河组天然气勘探为例[J].石油与天然气地质,2010,31(6):707-714.
    [6]
    蒋裕强,郭贵安,陈义才,等.蜀南河包场地区须家河组气藏成藏机理及成藏模式[J].石油实验地质,2010,32(4);314-318.
    [7]
    吕正祥.川西孝泉构造上三叠统超致密储层演化特征[J]. 都理工大学学报(自然科学版),2005,32(1):22-26.
    [8]
    吕正祥,刘四兵.川西须家河组超致密砂岩成岩作用与相对优质储层形成机制[J].岩石学报,2009,25(10):2373-2383.
    [9]
    Xu Zhangyou,Zhang Xiaoyu,Wu Shenghe,et al.Genesis of the low-permeability reservoir bed of Upper Triassic Xujiahe Formation in Xinchang gas field,Western Sichuan Depression[J].Petroleum Science,2008,5 (3):230-237.
    [10]
    苏永进,唐跃刚,张世华,等.川西坳陷上三叠统天然气成藏主控因素及形成模式[J].石油与天然气地质,2010,31(1):107-113.
    [11]
    冯明石,刘家铎,孟万斌,等.四川盆地中西部须家河组储层特征与主控因素[J].石油与天然气地质,2009,30(6):713-719.
    [12]
    Folk R L.Petrology of sedimentary rocks[M].Austin:Hemphill,1968:107.
    [13]
    Dickinson W,Suczec C.Plate tectonics and sandstone compositions[J].AAPG Bulletin,1979,63:2164-2182.
    [14]
    Houseknecht D W.Assessing the relative importance of compaction processes and cementation to reduction of porosity in sandstones[J].AAPG Bulletin,1987,71:633-642.
    [15]
    Ehrenberg S N.Assessing the relative importance of compaction processes and cementation to reduction of porosityin sandstones:Discussion; Compaction and porosity evolution of Pliocene sandstones,Ventura Basin,California:Discussion[J].AAPG Bulletin,1989,77:1260-1286.
    [16]
    Morad S,Al-Ramadan K,Ketzer J M,et al.The impact of diagenesis on the heterogeneity of sandstone reservoirs:A review of the role of depositional facies and sequence stratigraphy[J].AAPG Bulletin,2010,94(8):1267-1309.
    [17]
    Beard D C,Weyl P K.Influence of texture on porosity and permeability of unconsolidated sand[J].AAPG Bulletin,1973,57(2):349-369.
    [18]
    Friedman I,O'Neil J R.Compilation of stable isotope fractionation factors of geochemical interest[G]//Fleischer M.Data of geochemistry.6th ed.Washington D C:USGS,1977:1-12.
    [19]
    Berger A,Gier S,Krois P.Porosity-preserving chlorite cements in shallow-marine volcanidasfic sandstones:Evidence from Cretaceous sandstones of the Sawan gas field,Pakistan[J].AAPG Bulletin,2009,93(5):595-615.
    [20]
    Billault V,Beaufort D,Baronet A,et al.A nanopetrographic and textural study of grain-coating chlorites in sandstone reservoirs[J].Clay Minerals,2003,38(3):315-328.
    [21]
    黄思静,谢连文,张萌,等.中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J].成都理工大学学报(自然科学版),2004,31(3):273-281.
    [22]
    Worden R H,Morad S.Clay minerals in sandstones:Controls on formation,distribution and evolution[M]//Worden R H,Morad S.Clay mineral cements in sandstones.Oxford:Blackwell Science,2003:1-41.
    [23]
    Fisher Q J,Knipe R,Worden R H.Micro-structures of deformed and non-deformed sandstones from the North Sea:Implication for the origins of quartz cement in sandstones[G]//Worden R H,Morad S.Quartz cementation in sandstones.Oxford:Blackwell Science,2000:129-146.
    [24]
    Pittman E D,Lumsden D N.Relationship between chlorite coatings on quartz grains and porosity,Spiro sand,Oklahoma[J].Journal of Sedimentary Petrology,1968,38:668-670.
    [25]
    Luo J L,Morad S,Salem A,et al.Impact of diagenesis on reservoir quality evolution in fluvial and lacustring-deltaic sandstones:Evidence from Jurassic and Triassic sandstones from the Ordos Basin,China[J].Journal of Petroleum Geology,2009,32(1):79-102.
    [26]
    Wilkinson M,Haszeldine R S,Ellam R M,et al.Hydrocarbon filling history from diagenesis evidence:Brent Group,UK North Sea[J].Marine and Petroleum Geology,2004,21:443-455.
    • Relative Articles
    • Supplements(0)
    • Cited By

  • Cited by

    Periodical cited type(1)

    1. 马晓潇，黎茂稳，胡克珍，陶国亮，钱门辉，曹婷婷，刘鹏，李志明，蒋启贵，李政. 渤海湾盆地济阳坳陷古近系异常高压成因及其与陆相页岩油富集的关系. 石油实验地质. 2023(01): 145-156 . 本站查看

    Other cited types(0)

  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-052024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-04010203040
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 17.4 %FULLTEXT: 17.4 %META: 71.0 %META: 71.0 %PDF: 11.5 %PDF: 11.5 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 7.6 %其他: 7.6 %其他: 0.1 %其他: 0.1 %Russian Federation: 0.1 %Russian Federation: 0.1 %Tulsa: 0.3 %Tulsa: 0.3 %[]: 0.2 %[]: 0.2 %三门峡: 0.1 %三门峡: 0.1 %上海: 0.7 %上海: 0.7 %东莞: 0.1 %东莞: 0.1 %东营: 1.8 %东营: 1.8 %临汾: 0.2 %临汾: 0.2 %乌鲁木齐: 0.1 %乌鲁木齐: 0.1 %克拉玛依: 0.2 %克拉玛依: 0.2 %兰州: 0.3 %兰州: 0.3 %北京: 5.8 %北京: 5.8 %南京: 0.3 %南京: 0.3 %南平: 0.1 %南平: 0.1 %台州: 0.7 %台州: 0.7 %呼和浩特: 0.1 %呼和浩特: 0.1 %哥伦布: 0.1 %哥伦布: 0.1 %唐山: 0.1 %唐山: 0.1 %圣何塞: 0.1 %圣何塞: 0.1 %城南: 0.1 %城南: 0.1 %大同: 0.4 %大同: 0.4 %大庆: 0.4 %大庆: 0.4 %天津: 0.6 %天津: 0.6 %宁德: 0.2 %宁德: 0.2 %宣城: 0.4 %宣城: 0.4 %巴音郭楞: 0.3 %巴音郭楞: 0.3 %张家口: 1.6 %张家口: 1.6 %成都: 1.0 %成都: 1.0 %扬州: 0.1 %扬州: 0.1 %无锡: 2.3 %无锡: 2.3 %昆明: 0.1 %昆明: 0.1 %晋城: 0.1 %晋城: 0.1 %朝阳: 0.4 %朝阳: 0.4 %杭州: 0.6 %杭州: 0.6 %格兰特县: 0.1 %格兰特县: 0.1 %武汉: 1.7 %武汉: 1.7 %沈阳: 0.3 %沈阳: 0.3 %法尔肯施泰因: 0.1 %法尔肯施泰因: 0.1 %济南: 0.6 %济南: 0.6 %海口: 0.2 %海口: 0.2 %海得拉巴: 1.3 %海得拉巴: 1.3 %深圳: 0.2 %深圳: 0.2 %湖州: 0.1 %湖州: 0.1 %滨州: 0.2 %滨州: 0.2 %漯河: 0.3 %漯河: 0.3 %盘锦: 0.2 %盘锦: 0.2 %石家庄: 0.3 %石家庄: 0.3 %福州: 0.1 %福州: 0.1 %秦皇岛: 0.2 %秦皇岛: 0.2 %芒廷维尤: 28.4 %芒廷维尤: 28.4 %芝加哥: 0.6 %芝加哥: 0.6 %莆田: 0.1 %莆田: 0.1 %莫斯科: 0.6 %莫斯科: 0.6 %衡水: 0.2 %衡水: 0.2 %衢州: 0.6 %衢州: 0.6 %西宁: 15.0 %西宁: 15.0 %西安: 1.6 %西安: 1.6 %诺沃克: 0.8 %诺沃克: 0.8 %贵阳: 0.3 %贵阳: 0.3 %运城: 2.5 %运城: 2.5 %遵义: 0.1 %遵义: 0.1 %郑州: 0.3 %郑州: 0.3 %重庆: 0.3 %重庆: 0.3 %金华: 0.4 %金华: 0.4 %锦州: 0.4 %锦州: 0.4 %长春: 0.1 %长春: 0.1 %长沙: 12.5 %长沙: 12.5 %阿什本: 0.2 %阿什本: 0.2 %青岛: 0.1 %青岛: 0.1 %首尔: 0.2 %首尔: 0.2 %黄南: 0.1 %黄南: 0.1 %龙岩: 0.1 %龙岩: 0.1 %其他其他Russian FederationTulsa[]三门峡上海东莞东营临汾乌鲁木齐克拉玛依兰州北京南京南平台州呼和浩特哥伦布唐山圣何塞城南大同大庆天津宁德宣城巴音郭楞张家口成都扬州无锡昆明晋城朝阳杭州格兰特县武汉沈阳法尔肯施泰因济南海口海得拉巴深圳湖州滨州漯河盘锦石家庄福州秦皇岛芒廷维尤芝加哥莆田莫斯科衡水衢州西宁西安诺沃克贵阳运城遵义郑州重庆金华锦州长春长沙阿什本青岛首尔黄南龙岩

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
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (3576) PDF downloads(1024) Cited by(1)
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return