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

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.
引用本文: 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.
LV ZhengXiang, LIU SiBing. Ultra-tight sandstone diagenesis and mechanism for the formation of relatively high-quality reservoir of Xujiahe Group in western Sichuan[J]. Acta Petrologica Sinica, 2009, 25(10): 2373-2383.
Citation: LV ZhengXiang, LIU SiBing. Ultra-tight sandstone diagenesis and mechanism for the formation of relatively high-quality reservoir of Xujiahe Group in western Sichuan[J]. Acta Petrologica Sinica, 2009, 25(10): 2373-2383.

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

Ultra-tight sandstone diagenesis and mechanism for the formation of relatively high-quality reservoir of Xujiahe Group in western Sichuan

  • 川西须家河组砂岩是我国重要的天然气储层和产层,同时也是我国埋藏深度最大和最为致密的碎屑岩储层之一,在其超致密背景下发育有对天然气聚集有利的相对优质储层。须家河组砂岩埋藏后经历了复杂的成岩作用,相对优质储层中次生孔隙与原生孔隙并存。本文基于对川西须家河组超致密砂岩的岩石学、矿物学、地球化学和其它储层特征研究,总结了川西深埋藏条件下须家河组砂岩的成岩作用特征及其相对优质储层的形成机制。
  • 加载中
  • [1]

    Appert O.1998. Editorial:Special issue on production of reservoir fluids in frontier conditions:Revue de L\' Institut Francais du Pe\'trole,53(3):249-252

    [2]

    Bj(o)rlykke K,Nedkvitne T,Ramm M et al.1992. Diagenetic processes in the Brent Group(Middle Jurassic)reservoirs of the North Sea:An overview.Morton AC,Haszeldine AS,Giles MR et al.Geology of the Brent group(Special Publication Vol.63).London:Geological Society,265-289

    [3]

    Bethke CM.1986. Inverse hydrologic analysis of the distribution and origin of Gulf Coast-type geopressured zones.Journal of Geophysical Research,91:6535-6545

    [4]

    Billault V,Beaufort D,Baronnet A et al.2003. A nanopetrographic and textural study of grain-coating chlorites in sandstone reservoirs.ClayMinerals,38:315-328

    [5]

    Baker JC,Havord PJ,Martin KR et al.2000. Diagenesis and petrophysics of the Early Permian Moogooloo Sandstone,southern Carnarvon Basin,Western Australia.AAPG Bulletin,84(2):250-265

    [6]

    Bj(o)rlykke K.1993. Fluid flow in sedimentary basins:Sedimentary Geology,86:137-158

    [7]

    Cai JG,Zhang ZH,Zhu XM,Xie ZH,Li YX,LiuHJ and Yuan DS.2003. Hydrocarbon filling and chemical diagenesis evolution of the clastic reservoir of the Paleogene in Dongying Sag.Petroleum Exploration and Development,30(3):79-83(in Chinese with English abstract)

    [8]

    Du X,Zheng HY and Jiao XQ.1995. Abnormal pressure and hydrocarbon accumution.EARTH SCIENCE FRONTIERS,2(2-3):137-147(in Chinese with English abstract)

    [9]

    de Ros LF,Morad S and Palm PSG.1994. The role of detrital composition and climate on the diagenetic evolution of continental molasses:Evidence from the Cambro-Ordovician Guaritas Sequence,southern Brazil.Sedimentary Geology,92:197-228

    [10]

    Ehrenberg SN.1990. Relationship between diagenesis and reservoir quality in sandstone of the Garn Formation,Haltenbanken,mid-Norwegian continental shelf.AAPG Bulletin,74:1538-1558

    [11]

    Ehrenberg SN and Boassen T.1993. Factors controlling permeability variation in sandstones of the Garn Formation in Trestakk field,Norwegian continental shelf.Journalof Sedimentary Petrology,63:929-944

    [12]

    Ehrenberg SN,DallandA,AmundsenH EF et al.1998. Origin of chlorite enrichment and neodymium isotopic anomalies in Halternbanken sandstones.Marine and Petroleum Geology,15:403-425

    [13]

    Ehrenberg SN.1993. Preservation of anomalously high porosity in deeply buried sandstones by grain-coating chlorite:Examples from the Norwegian Continental Shelf.AAPG Bulletin,77(7):1260-1286

    [14]

    Gong ZS,Li ST,Xie TJ et al.1997. The basin analysis and oil and gas accumulation of the continental margin of the northern South China Sea,China,Beijing:Scientific Publishing House,222-256(in Chinese with English abstract)

    [15]

    Grigsby and Jeffry D.2001. Origin and growth mechanism of authigenic chlorite in sandstones of the lower Vicksburg Formation,South Texas.Journal of Sedimentary Research,71:27-36

    [16]

    Giles MR and RB de-Boer.1990. Origin and significance of redistributional secondary porosity:Marine and Petroleum Geology,7:378-397

    [17]

    Huang SJ,Wu WH,Liu J,Shen LC and Huang CG.2003. Generation of Secondary Porosity by Meteoric Water during Time of Subaerial Exposure:An Example from Yanchang Formation Sandstone of Triassic of Ordos Basin.Earth Science-Journal of China University of Geosciences,28(4):419-424(in Chinese with English abstract)

    [18]

    Huang SJ,Xie LW,Zhang M,Wu WH,Shen LC and Liu J.2004. Formation mechanism of authigenic chlorite and relation to preservation of porosity in nonmarine Triassic reservoir sandstones,Ordos Basin and Sichuan Basin,China.Journal of Chengdu University of Technology(Science & Technology Edition),31(3):273-281(in Chinese with English abstract)

    [19]

    Hillier S,FallickA E and Matter A.1996. Origin of pore-lining chlorite in the Aeolian Rotliegend of Northern Germany.Clay Minerals,31:153-171

    [20]

    Hilliers,Wilson MJ,Merriman RJ et al.2006. Clay mineralogy of the old red sandstone claymineralogy of the old red sandstone and Devonian sedimentary rocks of Wales,Scotland and England.Clay Minerals,41:433-471

    [21]

    Kugler RL and McHugh A.1990. Regional diagenetic variation in Norphlet Sandstone:Implications for reservoir quality and the origin of porosity.Transaction of the Gulf Coast Association of Geological Societies,40:411-423

    [22]

    Kupecz JA,Gluyas J and Bloch S.1997. Reservoir Quality Prediction in Sandstones and Carbonates-An Overview.AAPG Memoir,69:Vii-xxiv

    [23]

    Li J,Zhang L,Cao Z and Zhang LQ.1999. Formation mechanism for deep abnormal pores of Dagang exploration area.China Petrleum Exploration,4(4):20-23(in Chinese with English abstract)

    [24]

    Li HJ,Wu TR,Wu B,Zhu L and Guo GL.2004. Distribution and controlling factors of high quality clastic deeply buried reservoirs in China.Geological Science and Technology Information,23(4):76-82(in Chinese with English abstract)

    [25]

    Lanson B,Beaufort D,Berger G et al.2002. Authigenic kaolin and illitic minerals during burial diagenesis of sandstones:A review.Clay Minerals,37:1-22

    [26]

    Lü ZX and Qing C.2001. Geological factors affecting reservoir permeability of the Upper Shaximiao Formation in the Xinchang gas field,western Sichuan.Sedimentary Geology and Tethyan Geology,21(2):57-63(in Chinese with English abstract)

    [27]

    Lü ZX.2005. Evolutionary characteristics of Upper Triassic reservoir in Xiaoquan structure in West Sichuan,China.Journal of Chengdu University of Technology(Science & Technology Edition),32(1):22-26(in Chinese with English abstract)

    [28]

    Liu BJ.1980. Sedimentary petrology.Beijing:Geological Publishing House(in Chinese with English abstract)

    [29]

    McBride SM,Frank PC and Larese AE.1987. Chlorite grain coats and preservation of primary porosity in deeply buried Springer Formation and Lower Morrowan sandstone,southeastern Anadako basin,Oklahoma.APPG Bulletin,71:994

    [30]

    Miao JY,Zhu ZQ,Liu WR and Lu HY.2000. Relationship between temperature-pressure and secondary pores of deep reservoirs in eogene at Jiyang Depression.ACTA PETROLEI SINICA,21(3):36-40(in Chinese with English abstract)

    [31]

    Nedkvitne T,Karlsen DA,Bj(o)rlykke K et al.1993. Relationship between reservoir diagenetic evolution and petroleum emplacement in the Ula field,North Sea.Marine and Petroleum Geology,10:255-270

    [32]

    Osborne MJ and Swarbrick RE.1999. Diagenesis in North Sea HPHT clastic reservoirs:Consequences for porosity and overpressure prediction.Marineand Petroleum Geology,16:337-353

    [33]

    Pittman ED,Larese RE and Heald MT.1992. Clay coats:Occurrence and relevance to preservation of porosity in sandstones Houseknecht D W,Pittman E D.Origin,diagensis,and petrophysics of clay minerals in sandstones(Special Publication Vol.47).Society of Economic Paleontologists and Mineralogist,241-255

    [34]

    Ryan PC and jr Reynolds RC.1996. The origin and diagenesis of grain coating sepentine-chlorites in Tuscaloosa Formation sandstone,U.S.Gulf Coast.American Mineralogist,81:213-225

    [35]

    Richard H,Worden and SadoonMorad.2003. ClayMineral Cements in Sandstones.Oxford:BlackwellScience Ltd.

    [36]

    Shi JA and Wang Q.1995. A disscussion on main controlling factors on the properties of clastic gas reservoirs.ACTA SEDIMENTOLOGICA SINICA,13(2):128-139(in Chinese with English abstract)

    [37]

    Souza RS,de Ros LF and Morad S.1995. Dolomite diagenesis and porosity preservation in lithic reservoirs:Carm-polis member,Sergipe-Alagoas basin,northeastern Brazil.AAPG Bulletin,79:725-748

    [38]

    Salman Bloch,Robert H Lander,Linda Bonnel et al.2002. Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and Predictability.AAPG Bulletin,86:301-328

    [39]

    Sun ZL,Huang SJ,Zhang YX,Wang QD,Bao SX and Sun ZX.2008. Origin and diagenesis of authigenic chlorite within the sandstone reservoirs of Xujiahe formation,Sichuan Basin,China.ACTA SEDIMENTOLOGICA SINICA,26(3):459-468(in Chinese with English abstract)

    [40]

    Wilson MD.1992. Inherited grain-rimming clays in sandstones from eolian and shelf environments:Their origin and control on reservoir properties Houseknecht D W,Pittman E D.Origin,diagensis,and petrophysics of clay minerals in sandstones(Special Publication Vol.47).Society of Economic Paleontologists and Mineralogist,209-225

    [41]

    Wilkinson M,Darby D,Haszedine RS et al.1997. Secondary porosity generation during deep burial associated with overpressure leak-off:Fulmar Formation,United Kingdom Central Graben.AAPG Bulletin,81:803-813

    [42]

    Worden RH,Needham SJ,Cuadros J et al.2006. The worm gut:A natural claymineral factory and a possible cause of diagenetic grain coats in sandstones.Journal of Geochemical Exploration,89:428-431

    [43]

    Wang YC.1999. Oil and gas reservoir evaluation.Beijing:Petroleum Industry Press(in Chinese with English abstract)

    [44]

    Wang YC,Zhou W,Zhu YM et al.1992. Tight fractured oil and gas reservoir.Beijing:Geological Publishing House(in Chinese with English abstract)

    [45]

    Yang XH,Ye JR,Sun YC,Zhou SK and Wu WL.1998. Diagenesis evolution and preservation of porosity in the member 2,Shahejie formation,Qi\' nan Fault-step zone.China Offshore Oil and Gas(geology),12(4):242-249(in Chinese with English abstract)

    [46]

    Zhai YH,Guo JH and Liu SG.1996. Study on the origine of clastic rocks reservoir in carboniferous from Tazhong area.JOURNAL OF MINERALOGY AND PETROLOGY,6(2):55-61(in Chinese with English abstract)

    [47]

    蔡进功,张枝焕,朱筱敏,谢忠怀,李艳霞,刘洪军,袁东山.2003.东营凹陷烃类充注与储集层化学成岩作用.石油勘探与开发,30(3):79-83

    [48]

    杜栩,郑洪印,焦秀琼.1995.异常压力与油气分布.地学前缘,2(2-3):137-147

    [49]

    龚再升,李思田,谢泰俊等.1997.南海北部大陆边缘盆地分析与油气聚集.北京:科学出版社,222-256

    [50]

    黄思静,武文慧,刘洁,沈立成,黄成刚.2003.大气水在碎屑岩次生孔隙形成中的作用--以鄂尔多斯盆地三叠系延长组为例.地球科学-中国地质大学学报,28(4):419-424

    [51]

    黄思静,谢连文,张萌,武文慧,沈立成,刘洁.2004.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.成都理工大学学报(自然科学版),31(3):273-281

    [52]

    李军,张林,曹中,张立勤.1999.大港探区深层异常孔隙成因机理.中国石油勘探,4(4):20-23

    [53]

    李会军,吴泰然,吴波,朱雷,郭光立.2004.中国优质碎屑岩深层储层控制因素综述.地质科技情报,23(4):76-82

    [54]

    吕正祥,卿淳.2001.川西新场气田上沙溪庙组储层渗透性的地质影响因素.沉积与特提斯地质,21(2):57-63

    [55]

    吕正祥.2005.川西孝泉构造上三叠统超致密储层演化特征.成都理工大学学报(自然科学版),32(1):22-26

    [56]

    刘宝珺.1980.沉积岩石学.北京:地质出版社,125-127

    [57]

    苗建宇,祝总祺,刘文荣,卢焕勇.2000.济阳坳陷下第三系温度、压力与深部储层次生孔隙的关系.石油学报,21(3):36-40

    [58]

    史基安,王琪.1995.影响碎屑岩天然气储层物性的主要控制因素.沉积学报,13(2):128-139

    [59]

    孙治雷,黄思静,张玉修,王庆东,包申旭,孙致学.2008.四川盆地须家河组砂岩储层中自生绿泥石的来源与成岩演化.沉积学报,26(3):459-468

    [60]

    王允诚.1999.油气储层评价.北京:石油工业出版社

  • 加载中
计量
  • 文章访问数:  7411
  • PDF下载数:  10682
  • 施引文献:  0
出版历程
刊出日期:  2009-10-31

目录