沉积盆地充填过程的计算机模拟及其软件
摘要
沉积盆地充填过程的计算机模拟可以提高我们对地质现象的认识,甚至提供了一种定量解释和预测地层形态和层序边界的途径,可以检验对潜在油气区带的预测以及石油地质条件的关系。同时计算机模拟也是一种经济、易用的方法,并可以由相应模拟软件直接得到可视化的模拟结果。层序地层学的出现为盆地充填分析提供了建立等时地层格架和进行沉积体系域分析的方法理论,有力地促进了沉积盆地充填模型和动力学过程的研究。基于不同模型发展起来的盆地充填模拟软件,有机的与层序地层学结合,使得层序地层学主要应用于地震和测井中的情况得到改变。采用更易为地质家认同的模拟模型和更加灵活的人机交互方式,以及发展反演模拟是沉积盆地充填过程计算机模拟的发展方向。
引文
[1]Harbaugh J W,Carter G Bonham.Computer Simulation in Geology[M].New York:John Wiley & Sons,1970,1-57.
[2]Cross T A,Lessenger M A.Sediment Volume Partitioning: Rationale for Stratigraphic Model Evalution and High-Resolution Stratigraphic Correlation[A].In:Gradstein F M,Sandvik K O,Milton N J.Sequence stratigraphy concepts and application.NEF Special Publication [C].1998,8:171-195.
[3]闫伟鹏,邓宏文,王红亮.层序地层学的计算机模拟研究进展[J].石油与天然气地质,2004,25(5):596-602.
[4]Tetzlaff D M.Clastic simulation model of clastic sedimentatary [J].AAPGBull,1986,79:655.
[5]Bitzer K,Harbaugh J W.DEPOSIM.a Mackintosh computer model for two-dimensional simulation of transport, deposition,erosion,and compaction of clastic sediments [J].Computer and Geosciences,1987,13(6):611-637.
[6]Klaus Bitzer.Two-dimensional simulation of clastic and carbonate sedimentation,consolidation,subsidence,fluid flow,heat flow and solute transport during the formation of sedimentary basins[J].Computers & Geosciences, 1999,25:431-447.
[7]A Quiquerez,P Allemand,G Dromart.DIBAFILL:a 3-D two-lithology diffusive model for basin infilling[J].Computer & Geosciences,2000,26:1029-1042.
[8]Griffiths C M.Sedsim Stratigraphic Forward Modeling. CSIRO Petroleum,2003,4.
[9]Cross T A,Lessenger M A.Construction and application of a stratigraphic inverse model[A].In J W Harbaugh,W L Watney,E C Rankey,et al.SEPM Special Publication 62 Numerical Experiments in Stratigraphy:Recent Advances in Stratigraphic and Sedimentologic Computer Simulations: SEPM(Society for Sedimentary Geology)[C]. 1999,69-83.
[10]Lessenger M A,Cross T A.An inverse stratigraphic simulation model is stratigraphic inversion possible[J].Exploration and Exploitation,1996,14:627-637.
[11]Burton R,Kendall C G St C,Lerche I.Out of our depth:onthe impossibility of fathoming eustasy from the stratigraphic record [J].EarthScience Reviews,1987,24:237-277.
[12]李翔.沉积盆地充填过程的计算机模拟研究[J].现代地质,1994,8(4):393-402.
[13]Tetzlaff D M,Harbaugh J W.Simulating clastic sedimentation [M].New York:Van Nostrand Reinhold,1989,203- 297.
[14]Flemings P B,Grotzinger J P.STRATA:Freeware for Solving Classic Stratigraphic Problems[J].GSA Today, 1996,6(12):1-7.
[15]Keyu Liu,Trent C K Liang,Lincoln Paterson et al. Computer simulation of the influence of basin physiography on condensed section deposition and maximum flooding [J].Sedimentary Geology,1998,122:181-191.
[16]Ulf Nordlund.FUZZIM:forward stratigraphic modeling made simple[J].Computers & Geosciences,1999,25:449- 456.
[17]Flemings P E,Jordan T E.A Synthetic Stratigraphic Model of Foreland Basin Development[J].Journal of Geophysical Research,1989,94:3851-3866.
[18]Jordan T E,Flemings P E.Large-Scale Stratigraphic Architecture, Eustatie Variation,and Unsteady Tectonism: A Theoretical Evaluation[J].Journal of Geophysical Research, 1991,96(B4):6681-6699.
[19]Flemings P E,Jordan T E.Stratigraphic Modeling of Foreland Basins..Interpreting Thrust Deformation and Lithosphere Rheology[J].Geology,1990,8:430-434.
[20]林畅松,李思田,任建业.断陷湖盆层序地层学研究和计算机模拟——以二连盆地乌里雅斯太断陷为例[J].地学前缘,1995,2(3-4):124-132.
[21]阮同军.硅质碎屑岩沉积层序三维计算机模拟系统[J].计算机应用研究,1996,6:47-49.
[22]胡受权.湖平面变化及物源供给对陆相层序影响机理的计算机模拟[J].断块油气田,2000,7(6):1-11.
[23]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375.
[24]林畅松,解习农,等.二维沉积层序计算机模拟研究[J].沉积学报,1998,16(2):68-73.
[2]Cross T A,Lessenger M A.Sediment Volume Partitioning: Rationale for Stratigraphic Model Evalution and High-Resolution Stratigraphic Correlation[A].In:Gradstein F M,Sandvik K O,Milton N J.Sequence stratigraphy concepts and application.NEF Special Publication [C].1998,8:171-195.
[3]闫伟鹏,邓宏文,王红亮.层序地层学的计算机模拟研究进展[J].石油与天然气地质,2004,25(5):596-602.
[4]Tetzlaff D M.Clastic simulation model of clastic sedimentatary [J].AAPGBull,1986,79:655.
[5]Bitzer K,Harbaugh J W.DEPOSIM.a Mackintosh computer model for two-dimensional simulation of transport, deposition,erosion,and compaction of clastic sediments [J].Computer and Geosciences,1987,13(6):611-637.
[6]Klaus Bitzer.Two-dimensional simulation of clastic and carbonate sedimentation,consolidation,subsidence,fluid flow,heat flow and solute transport during the formation of sedimentary basins[J].Computers & Geosciences, 1999,25:431-447.
[7]A Quiquerez,P Allemand,G Dromart.DIBAFILL:a 3-D two-lithology diffusive model for basin infilling[J].Computer & Geosciences,2000,26:1029-1042.
[8]Griffiths C M.Sedsim Stratigraphic Forward Modeling. CSIRO Petroleum,2003,4.
[9]Cross T A,Lessenger M A.Construction and application of a stratigraphic inverse model[A].In J W Harbaugh,W L Watney,E C Rankey,et al.SEPM Special Publication 62 Numerical Experiments in Stratigraphy:Recent Advances in Stratigraphic and Sedimentologic Computer Simulations: SEPM(Society for Sedimentary Geology)[C]. 1999,69-83.
[10]Lessenger M A,Cross T A.An inverse stratigraphic simulation model is stratigraphic inversion possible[J].Exploration and Exploitation,1996,14:627-637.
[11]Burton R,Kendall C G St C,Lerche I.Out of our depth:onthe impossibility of fathoming eustasy from the stratigraphic record [J].EarthScience Reviews,1987,24:237-277.
[12]李翔.沉积盆地充填过程的计算机模拟研究[J].现代地质,1994,8(4):393-402.
[13]Tetzlaff D M,Harbaugh J W.Simulating clastic sedimentation [M].New York:Van Nostrand Reinhold,1989,203- 297.
[14]Flemings P B,Grotzinger J P.STRATA:Freeware for Solving Classic Stratigraphic Problems[J].GSA Today, 1996,6(12):1-7.
[15]Keyu Liu,Trent C K Liang,Lincoln Paterson et al. Computer simulation of the influence of basin physiography on condensed section deposition and maximum flooding [J].Sedimentary Geology,1998,122:181-191.
[16]Ulf Nordlund.FUZZIM:forward stratigraphic modeling made simple[J].Computers & Geosciences,1999,25:449- 456.
[17]Flemings P E,Jordan T E.A Synthetic Stratigraphic Model of Foreland Basin Development[J].Journal of Geophysical Research,1989,94:3851-3866.
[18]Jordan T E,Flemings P E.Large-Scale Stratigraphic Architecture, Eustatie Variation,and Unsteady Tectonism: A Theoretical Evaluation[J].Journal of Geophysical Research, 1991,96(B4):6681-6699.
[19]Flemings P E,Jordan T E.Stratigraphic Modeling of Foreland Basins..Interpreting Thrust Deformation and Lithosphere Rheology[J].Geology,1990,8:430-434.
[20]林畅松,李思田,任建业.断陷湖盆层序地层学研究和计算机模拟——以二连盆地乌里雅斯太断陷为例[J].地学前缘,1995,2(3-4):124-132.
[21]阮同军.硅质碎屑岩沉积层序三维计算机模拟系统[J].计算机应用研究,1996,6:47-49.
[22]胡受权.湖平面变化及物源供给对陆相层序影响机理的计算机模拟[J].断块油气田,2000,7(6):1-11.
[23]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375.
[24]林畅松,解习农,等.二维沉积层序计算机模拟研究[J].沉积学报,1998,16(2):68-73.
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