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Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character

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文章导航 > 沉积学报  > 1999 >  17(2): 263-268
Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character[J]. 沉积学报, 1999, 17(2): 263-268.
引用本文: Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character[J]. 沉积学报, 1999, 17(2): 263-268.
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Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character

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  • 中图分类号: P618.130.21

    摘要
  • 摘要: Quartz cementation is a very important diagenetic event and main porosity-occluding factor in the reservoir sandstones in middle Jurassic i n North Sea. Petrological studies indicate the quartz cementation is limited in shallower burial depth and increases significantly at depth around 3.5 - 4 km. T he amount of quartz cement increases with burial depth from an average of approx imately 4%-5 vol% at 2.5 km to 17%-20 vol% at 4 km. Highest abundances of quartz cement exceeds 28% which has been found in the Ness Formation. Variations in qu artz cementation between different sandstone facies is minimal for any one forma tion, with exception of the generally lower quantities present in the heterolith ic sandstone. Homogenisation temperatures of fluid inclusion in quartz overgrowt h from the North Sea reservoirs indicate that few quartz cement occur below the temperature 70 ℃～80 ℃, the onset of large volume quartz cement starts at the temperatures higher than 90 ℃ which suggests the quartz cementation is temperat ure - dependent during progressing diagenesis of sandstones.
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    • 参考文献(34)
  • [1] Bjrlykke K，Brendsdal A, Diagenesis of the Brent Sandstones in the S tatfjord Field, North Sea[A] . In: Gautier D L, ed. Roles of organic matter in sediment diagenesis[C] . Society of Economic Palaeontologists and Mineralog ists, Special Publication, 38,1986.157～168
    [2] Bjrlykke K, Egeberg P K. Quartz cementation in sedimentary basins[J], American Association of Petroleum Geologists Bulletin,1993, 77: 1538～1548[ ZK)〗
    [3] Bjrlykke K, Aagaard P. Clay minerals in North Sea sandstones[A] . I n: Houseknecht D W, Pittman E D,eds. Origin, diagenesis, and petrophysics of cla y minerals in sandstones: SEPM Special Publication 1992. 47, 65～80
    [4] Bjrlykke K, Formation of secondary porosity: how important is it?[A], In: McDonald D A, Surdam R C,eds. Clastic diagenesis[C] American Associati on of Petroleum Geologists Memoir 1984.37: 277～286
    [5] Bjrlykke K, Nedkvitne T, Ramm M,Saigal G C. Diagenetic processes in the Brent Group (Middle Jurassic) reservoirs of the North Sea: an overview. In: Morton A C, et al.eds.Geology of the Brent Group. Geological Society Special Pub lication[C] ,1992. 61,263～287
    [6] Blatt H. Diagenetic processes in sandstones[A] . SEPM Special Publica tion 26[C] .1979.141～157
    [7] Bloch S. Effect of detrital mineral composition on reservoir quality. [A] . In: Wilson M D, ed. Reservoir quality assessment and prediction in clasti c rocks: SEPM Short course 30[C] .1994. 161～182
    [8] Bloch S, McGowen J H,Duncan J R，Brizzolara D W. Porosity prediction, prior to drilling, in sandstones of the Kekiktuk Formation (Mississippian), Nort h Slope of Alaska[J] . American Association of Petroleum Geologists Bulletin, 1990.74, 1 371～1 385
    [9] Bodnar R J, Binns P R, Hall D L. Synthetic fluid inclusions-VI. Quanti tative evaluation of the decrepitation behaviour of fluid inclusions in quartz a t one atmosphere confining pressure[J] . Journal of Metamorphic Geology,1989, 7 : 229～242
    [10] Dixon S A, Summers D M, Surdam R C. Diagenesis and preservation of po rosity in Norphlet Formation (Upper Jurassic), southern Alabama[J] . American A ssociation of Petroleum Geologists Bulletin, 1989, 73:707～728
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    [12] Ehernberg S N. Relationship between diagenesis and reservoir quality in sandstones of the Garm Formation, Haltenbanken, Mid-Norwegian continental she lf[J] American Association of Petroleum Geologists Bulletin,1990, 74:1 538～1 558
    [13] Ehrenberg S N, Nadeau P H. Formation of diagenetic illite in sandston es of the Garn Formation, Haltenbanken area, Mid-Norwegian Continental shelf[J]. Clay Minerals,1989, 24: 233～253
    [14] Giles M R, Stevenson S, Martin S V, Cannon S J. et al. The reservoir properties and diagenesis of Brent Group[A] . a regional perspective, In: Morto n A C. et al.es. Geology of the Brent Group[C] . Geological Society Special Pu blication, 1992,61, 289～328
    [15] Gluyas J C. Reduction and prediction of sandstone reservoir p otential, Jurassic, North Sea[J] . Philosophical Transactions of the Royal Soci ety of London, 1985, 315：187～202
    [16] Harris N B. Burial diagenesis of Brent sandstones: a study of Statfjo rd, Hutton and Lyell fields[A] . In： Morton A C et al.eds Geology of Brent Gro up[C] . Geological Society Special Publication, 1992,61,351～375
    [17] Harrison W J. Modelling fluid/rock interactions in sedimentary basins [A] . In: Cross T A. eds. Quantitative dynamic stratigraphy[C] . Prentice Hall, New York, 1989，195～231
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    [27] Robinson A. Gluyas J._duration of quartz cementation in sandstones, n orth Sea and Haltenbanken Basins[J] . Marine and Petroleum Geology, 1992.9,324 ～327
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    [33] Walderhaug O. Temperatures of quartz cementation in Jurassic sandston es from the Norwegian continental shelf- evidence from fluid inclusions[J] . J ournal of Sedimentary Research, 1994.64:311～323
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出版历程
  • 收稿日期:  1998-03-04
  • 刊出日期:  1999-06-10

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    Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character

    • 收稿日期: 1998-03-04
    • 刊出日期: 1999-06-10

    • 中图分类号: P618.130.21

    摘要: Quartz cementation is a very important diagenetic event and main porosity-occluding factor in the reservoir sandstones in middle Jurassic i n North Sea. Petrological studies indicate the quartz cementation is limited in shallower burial depth and increases significantly at depth around 3.5 - 4 km. T he amount of quartz cement increases with burial depth from an average of approx imately 4%-5 vol% at 2.5 km to 17%-20 vol% at 4 km. Highest abundances of quartz cement exceeds 28% which has been found in the Ness Formation. Variations in qu artz cementation between different sandstone facies is minimal for any one forma tion, with exception of the generally lower quantities present in the heterolith ic sandstone. Homogenisation temperatures of fluid inclusion in quartz overgrowt h from the North Sea reservoirs indicate that few quartz cement occur below the temperature 70 ℃～80 ℃, the onset of large volume quartz cement starts at the temperatures higher than 90 ℃ which suggests the quartz cementation is temperat ure - dependent during progressing diagenesis of sandstones.

    English Abstract

    Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character[J]. 沉积学报, 1999, 17(2): 263-268.
    引用本文: Quartz Cement in Middle Jurassic Reservoir Sandstones in North Sea. A Review. Part Ⅰ: Occurrence and Character[J]. 沉积学报, 1999, 17(2): 263-268.
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