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美国得克萨斯古生界和中生界鲕粒的微孔隙度

David C.Kopaska-Merkel 赖志云

David C.Kopaska-Merkel, 赖志云. 美国得克萨斯古生界和中生界鲕粒的微孔隙度[J]. 沉积学报, 1991, 9(4): 27-33.
引用本文: David C.Kopaska-Merkel, 赖志云. 美国得克萨斯古生界和中生界鲕粒的微孔隙度[J]. 沉积学报, 1991, 9(4): 27-33.
David C. Kopaska-Merkel, Lai Zhiyun. Microporosity in Ooids: Mesozoic and Palaeozoic of Texas, USA[J]. Acta Sedimentologica Sinica, 1991, 9(4): 27-33.
Citation: David C. Kopaska-Merkel, Lai Zhiyun. Microporosity in Ooids: Mesozoic and Palaeozoic of Texas, USA[J]. Acta Sedimentologica Sinica, 1991, 9(4): 27-33.

美国得克萨斯古生界和中生界鲕粒的微孔隙度

Microporosity in Ooids: Mesozoic and Palaeozoic of Texas, USA

  • 摘要: 本文所述的由1—5μm自形菱形方解石组成的微晶化鲕粒采自得克萨斯奥陶系—侏罗系的鲕粒灰岩和泥粒灰岩,其中:露头样品4个,岩心样品3个,岩屑样品7个。微晶化鲕粒的孔隙度可大于15%,渗透率为1毫达西.鲕粒的微晶化不是由淋滤作用所引起,而是在矿物稳定化过程中由文石转化而成方解石。
  • [1] (1) Ahr W.M., Faucette R.C. and SteCfensen C.K 1984, Gulf Coast Trans.. V.33, p.107-117.

    (2) Bathurst R.G:C., 1976. Carbonate sediments and their diagenesis. Elsevier, Amsterdam.p.658.

    (3) Daviea P.J.and MartinK、,1976, Geology, V.4, p.i20-122.

    (4) Folk R L,1974, Jour of Sed.Petrology,.V.44, p.40-53

    (5) Folk R.L., and Land L.S., 1975, A.A.P.G. Bu11.V.59, p.60-68.

    (6) Friedman G.M., 1964,Jour of Sed petrology, V.34, p.777-813.

    (7) Friedman G.M.and Sanders J.E., 1978. Principles of Sedimentology. John Wiley and Sons, New York, 792p

    (8) Keith B.D.and Pittman E.D., 1983, A.A.P.G. Bull., V.67, p.1391-99.

    (9) Kopaska-Merkel D.C.,1985. A.A.P.G. Bull., V.69, p.275

    (10) Kopaska-Merkel D.C.Amthor J. E. and Friedman G. M.,1987, Notes on the use of a mercury porosimeter (Micromerities Pore Sizer 9305): Northeastern Science Foundation Technical Report 1, 12p.

    (11) Moore C.H., 1984, The upper smackover of the Gulf Rim: depositional systems, diagenesis, porosity evolution and hydrocarbon production, in; Ventress W.P.S.and others, eds., The Jurassic of the Gulf Rim, proceedings of the third annual research conference, Gulf coast section, Soc. Econ. Paleontologists Mineralogists Foundation, p.283-307.

    (12) Moore C.H.and Drvckman Y., 1981, A.A.P.G.Bull., V.65, p.597-628.

    (13) Pluim S.B., Painter P.G., Bucber E.J.and Chaky A.L., 1985. A.A.P.G.Bull.. V.69, p.296.

    (14) Purdy E.G., 1963, J.Geology, V.71,p.3 i4-355

    (15) Walkden G.M.and Berry J.R., 1984, Sedimentology. V.31,p.251-267.

    (16) Wardlaw N.C., 1976, Bull. V.60.p.245-257.

    (17) Wilkinsoun B.H., I982, Journal of Geological Education, V.30, p.189-203

    (18) Wilkinson B.H., Buczynski C.and Owen R.M., 1984, Jour.of Sed. Petrology, V.54, p.932-947.
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出版历程
  • 收稿日期:  1988-04-14
  • 刊出日期:  1991-12-10

目录

    美国得克萨斯古生界和中生界鲕粒的微孔隙度

    摘要: 本文所述的由1—5μm自形菱形方解石组成的微晶化鲕粒采自得克萨斯奥陶系—侏罗系的鲕粒灰岩和泥粒灰岩,其中:露头样品4个,岩心样品3个,岩屑样品7个。微晶化鲕粒的孔隙度可大于15%,渗透率为1毫达西.鲕粒的微晶化不是由淋滤作用所引起,而是在矿物稳定化过程中由文石转化而成方解石。

    English Abstract

    David C.Kopaska-Merkel, 赖志云. 美国得克萨斯古生界和中生界鲕粒的微孔隙度[J]. 沉积学报, 1991, 9(4): 27-33.
    引用本文: David C.Kopaska-Merkel, 赖志云. 美国得克萨斯古生界和中生界鲕粒的微孔隙度[J]. 沉积学报, 1991, 9(4): 27-33.
    David C. Kopaska-Merkel, Lai Zhiyun. Microporosity in Ooids: Mesozoic and Palaeozoic of Texas, USA[J]. Acta Sedimentologica Sinica, 1991, 9(4): 27-33.
    Citation: David C. Kopaska-Merkel, Lai Zhiyun. Microporosity in Ooids: Mesozoic and Palaeozoic of Texas, USA[J]. Acta Sedimentologica Sinica, 1991, 9(4): 27-33.
    参考文献 (1)

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