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FENG ZHISHENGup, FAN GUOHUAup2com . 1990: MODIFIED MONTE CARLO INVERSION METHOD AND ITS APPLICATION IN THE INVERSION OF MAGNETOTOL-LURIC SOUNDING DATA. Acta Seismologica Sinica, 12(3): 292-298.
Citation: FENG ZHISHENGup, FAN GUOHUAup2com . 1990: MODIFIED MONTE CARLO INVERSION METHOD AND ITS APPLICATION IN THE INVERSION OF MAGNETOTOL-LURIC SOUNDING DATA. Acta Seismologica Sinica, 12(3): 292-298.
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MODIFIED MONTE CARLO INVERSION METHOD AND ITS APPLICATION IN THE INVERSION OF MAGNETOTOL-LURIC SOUNDING DATA

  • 1. Seismological Bureau of Jiangsu Province; 2. Instituted of Geophysics, State Seismological Bureau

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  • Published Date: September 01, 2011
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  • In this paper,we combine the Jones' Monte Carlo inversion method with revised Mar-quardt inversion to get the new Monte Carlo inversion method. The method has advantages of high calculation speed and high precision of solution. It is actually a combination of random solution and directive solution. The authors processed the theoretical apparent resistivity data and actual apparent resistivity data using the new Monte Carlo inversion program,and a large number of models with high fitting degree,therefore obtaining the range of solution.
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    • References (1)
  • [1] Jupp. D. L. B., and Vozoff, K., 1975. Stable iterative methods for the inversion of geophysical data.Geophys. J. R. Astr. Soc., 42, 957—976.

    [2] 陈明生、陈乐寿、王天生、白改先,1983. 用改进的广义逆矩阵方法解释大地电磁测深及电测深资料.地球物理学报,26, 390—400.

    [3] Anderssen, R. S., 1970. The character of non—niqueness in the conductivity modelling problem for the earth. Pure Appl. Geophys., 80, 238—259.

    [4] Hermance, J. F. and Grillot, L. R., 1974. Constraints on temperatures beneath Iceland from magnetotel—luric data. Phys. Earth Plan. Int., 8, 1—12.

    [5] Jones, A. G, and Hutton, R., 1979. A multistation magnetotelluric study in southern Scotland——II,Monte—Carlo inversion of the data its geophysical and tectonic implication. Geophys. J. R. Astr. Soc., 56. 351—368.

    [1] Jupp. D. L. B., and Vozoff, K., 1975. Stable iterative methods for the inversion of geophysical data.Geophys. J. R. Astr. Soc., 42, 957—976.

    [2] 陈明生、陈乐寿、王天生、白改先,1983. 用改进的广义逆矩阵方法解释大地电磁测深及电测深资料.地球物理学报,26, 390—400.

    [3] Anderssen, R. S., 1970. The character of non—niqueness in the conductivity modelling problem for the earth. Pure Appl. Geophys., 80, 238—259.

    [4] Hermance, J. F. and Grillot, L. R., 1974. Constraints on temperatures beneath Iceland from magnetotel—luric data. Phys. Earth Plan. Int., 8, 1—12.

    [5] Jones, A. G, and Hutton, R., 1979. A multistation magnetotelluric study in southern Scotland——II,Monte—Carlo inversion of the data its geophysical and tectonic implication. Geophys. J. R. Astr. Soc., 56. 351—368.
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