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Volume 18 Issue 3
Jun 2007
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Article Contents
Yao Luo, Changli Yao. Forward Modeling of Gravity, Gravity Gradients, and Magnetic Anomalies due to Complex Bodies. Journal of Earth Science, 2007, 18(3): 280-286.
Citation: Yao Luo, Changli Yao. Forward Modeling of Gravity, Gravity Gradients, and Magnetic Anomalies due to Complex Bodies. Journal of Earth Science, 2007, 18(3): 280-286.

Forward Modeling of Gravity, Gravity Gradients, and Magnetic Anomalies due to Complex Bodies

Funds:

the National Natural Science Foundation of China 40374039

Program for New Century Excellent Talents in University NCET-04-0726

the Focused Subject Program of Beijing XK104910598

More Information
  • On the basis of the results of improved analytical expression of computation of gravity anomalies due to a homogeneous polyhedral body composed of polygonal facets, and applying the forward theory with the coordinate transformation of vectors and tensors, we deduced both the analytical expressions for gravity gradient tensors and for magnetic anomalies of a polygon, and obtained new analytical expressions for computing vertical gradients of gravity anomalies and vertical component of magnetic anomalies caused by a polyhedral body. And also we developed explicitly the complete unified expressions for the calculation of gravity anomalies, gravity gradient, and magnetic anomalies due to the homogeneous polyhedron. Furthermore, we deduced new analytical expressions for computing vertical gradients of gravity anomalies due to a finite rectangular prism by applying the newly obtained expressions for gravity gradient tensors due to a polyhedral target body. Comparison with forward calculation of models shows the correctness of these new expressions. It will reduce forward calculation time of gravity-magnetic anomalies and improve computational efficiency by applying our unified expressions for joint forward modeling of gravity-magnetic anomalies due to homogeneous polyhedral bodies.

     

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  • Barnett, C. T., 1976. Theoretical Modeling of the Magnetic and Gravitational Fields of an Arbitrarily Shaped Three-Dimensional Body. Geophysics, 41(6): 1353–1364 doi: 10.1190/1.1440685
    He, C. L., Zhong, B. S., 1988. A High Accuracy Forward Method for Gravity Anomaly of Complex Body. Computing Techniques for Geophysical and Geochemical Exploration, 10(2): 121–128 (in Chinese with English Abstract)
    Hou, Z. C., Liu, K. J., 1990. The Formulas and Procedures for Gravimagnetic Anomalies and Its Gradients. Geological Publishing House, Beijing (in Chinese)
    Li, X., Chouteau, M., 1998. Three-Dimensional Gravity Modeling in All Space. Surveys in Geophysics, 19(4): 339–368 doi: 10.1023/A:1006554408567
    Okabe, M., 1979. Analytical Expressions for Gravity Anomalies due to Homogeneous Polyhedral Bodies and Translations into Magnetic Anomalies. Geophysics, 44(4): 730–741 doi: 10.1190/1.1440973
    Pohánka, V., 1988. Optimum Expression for Computation of the Gravity Field of Homogeneous Polyhedral Body. Geophysical Prospecting, 36: 733–751 doi: 10.1111/j.1365-2478.1988.tb02190.x
    Tian, Q. N., Wu, W. L., Guan, Z. N., 2001. Interaction Inversion for 3D Gravity and Magnetic Anomalous Bodies with Arbitrary Shape. Computing Techniques for Geophysical and Geochemical Exploration, 23(2): 125–129 (in Chinese with English Abstract)
    Wang, B. H., Lin, S. B., Deng, Y. Q., 1980. Magnetic Fields of Uniformly Magnetized Polyhedra. Chinese J. Geophys., 23(4): 415–426 (in Chinese with English Abstract)
    Yao, C. L., Guan, Z. N., 1997. Computation of Magnetic Gradients due to Three-Dimensional Bodies. Science in China (Ser. D), 40(3): 293–299 doi: 10.1007/BF02877538
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