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DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE

Year 1986, Volume: 105-106 Issue: 105-106, 106 - 133, 01.10.1986

Abstract

Computer modelling, using Manik Talwani's method to determine the two dimensions of an ore
body is described. It is shown that quite accurate determination of the two dimensions of ore body is possible with such
application. It is suggested that such applications could be very useful for better programming of drilling and better estimation
of ore bodies in chromite.

References

  • 1 - Affleck, J., 1958, Interrelationships between magnetic anomaly components: Geophysics, 23, 738-748.
  • 2 - Bott, M.H.P., 1963, Two methods applicable to computer for evaluating magnetic anomalies due to finite three dimensinal bodies: Geophys. Prosp., l1, 292-299,
  • 3 - Gay, S.P., J.r,. 1963, Standard curves for interpretation of magnetic anomalies over long tabular bodies: Geophysics, 28, 161-200.
  • 4 - Henderson, R. G., ve Allingham, J. W., 1964, Magnetization of an inhomogencous laccolith calculated on a digital computer, in computers in the mineral industries, part 2: Stanford University publications, Geol. Sciences, 9, 481-497.
  • 5 - Herşey, J. B., 1962, Findings made during the June 1961 cruise of Chain to the Puerto Rico Trench and Caryn Seamount: Jour. Geophys. Res., 67, 1109-1116.
  • 6 - Miller, E.T. ve Eving, M., 1956, Geomagnetic measurements in the Gulf of Mexico and in the vicinity of Caryn Peak: Geophysics, 21, 406-432.
  • 7 - Steenland, N. C., 1962, Gravity and aeromagnetic exploralion in the Paradox Basin: Geophysics, 27, 73-89.
  • 8 - Talwani, M. ve Heirtzler, J.R., 1964, Computation of magnetic anomalies caused by two dimensional structures of arbitrary shape, in computer in the mineral industries, part 1: Stanford University publications, Geol, Sciences, 9, 464-480.
  • 9 - Thyssen Bornemisza, S. ve Stackler, W. F., 1956, Observing vertical gravity gradient: Geophysics, 21, 771-779. 1962, The average horizontal gravity gradient: Geophysics, 27, 714-715.
  • 10 - Vacquier, V., 1963, A machine method for computing the magnitude and the direction of magnetization of a uniformly magnetized body from its shape and a magnetic survey: Proc. Benedum Earth Magnetism Symposium 1962, University of Pittsburgh press.
  • 11 - , Steenland, N.C., Henderson, R.G., ve Zietz, 1., 1951, Interpretation of aeromagnetic maps:Geol. Soc. Amer., Mem., 47.
  • 12 - Vogel, A., 1963, The application of electronic computers to the calculation of effective magnetization: Geophys. Prosp., U, 51-58.
  • 13 - Werner, S., 1963, interpretation of magnetic of anomalies at sheetlike bodies: Sveriges Geologiska Undersockning, Arsbok, 43.
  • 14 - Worzel, J. L., 1959, Continuous gravity measurements on a surface ship with the Graf Sea Gravimeter: Jour. Geophys, Res., 64, 1299-1315.
  • 15 - Zietz, I. ve Henderson, R.G., 1956, A preliminary report on model Studies of magnetic anomalies of three dimensional bodies: Geophysics, 21, 794-814.
  • 16 - Talwani, M., 1965, Computation with the help of a digital computer of magnetic anomalies caused by bodies of arbitrary shape: Geophysics, 5 (October, 1965), 797-817, 11 figs.
Year 1986, Volume: 105-106 Issue: 105-106, 106 - 133, 01.10.1986

Abstract


References

  • 1 - Affleck, J., 1958, Interrelationships between magnetic anomaly components: Geophysics, 23, 738-748.
  • 2 - Bott, M.H.P., 1963, Two methods applicable to computer for evaluating magnetic anomalies due to finite three dimensinal bodies: Geophys. Prosp., l1, 292-299,
  • 3 - Gay, S.P., J.r,. 1963, Standard curves for interpretation of magnetic anomalies over long tabular bodies: Geophysics, 28, 161-200.
  • 4 - Henderson, R. G., ve Allingham, J. W., 1964, Magnetization of an inhomogencous laccolith calculated on a digital computer, in computers in the mineral industries, part 2: Stanford University publications, Geol. Sciences, 9, 481-497.
  • 5 - Herşey, J. B., 1962, Findings made during the June 1961 cruise of Chain to the Puerto Rico Trench and Caryn Seamount: Jour. Geophys. Res., 67, 1109-1116.
  • 6 - Miller, E.T. ve Eving, M., 1956, Geomagnetic measurements in the Gulf of Mexico and in the vicinity of Caryn Peak: Geophysics, 21, 406-432.
  • 7 - Steenland, N. C., 1962, Gravity and aeromagnetic exploralion in the Paradox Basin: Geophysics, 27, 73-89.
  • 8 - Talwani, M. ve Heirtzler, J.R., 1964, Computation of magnetic anomalies caused by two dimensional structures of arbitrary shape, in computer in the mineral industries, part 1: Stanford University publications, Geol, Sciences, 9, 464-480.
  • 9 - Thyssen Bornemisza, S. ve Stackler, W. F., 1956, Observing vertical gravity gradient: Geophysics, 21, 771-779. 1962, The average horizontal gravity gradient: Geophysics, 27, 714-715.
  • 10 - Vacquier, V., 1963, A machine method for computing the magnitude and the direction of magnetization of a uniformly magnetized body from its shape and a magnetic survey: Proc. Benedum Earth Magnetism Symposium 1962, University of Pittsburgh press.
  • 11 - , Steenland, N.C., Henderson, R.G., ve Zietz, 1., 1951, Interpretation of aeromagnetic maps:Geol. Soc. Amer., Mem., 47.
  • 12 - Vogel, A., 1963, The application of electronic computers to the calculation of effective magnetization: Geophys. Prosp., U, 51-58.
  • 13 - Werner, S., 1963, interpretation of magnetic of anomalies at sheetlike bodies: Sveriges Geologiska Undersockning, Arsbok, 43.
  • 14 - Worzel, J. L., 1959, Continuous gravity measurements on a surface ship with the Graf Sea Gravimeter: Jour. Geophys, Res., 64, 1299-1315.
  • 15 - Zietz, I. ve Henderson, R.G., 1956, A preliminary report on model Studies of magnetic anomalies of three dimensional bodies: Geophysics, 21, 794-814.
  • 16 - Talwani, M., 1965, Computation with the help of a digital computer of magnetic anomalies caused by bodies of arbitrary shape: Geophysics, 5 (October, 1965), 797-817, 11 figs.
There are 16 citations in total.

Details

Primary Language English
Subjects Engineering
Journal Section Articles
Authors

Doğan Aydal This is me

Publication Date October 1, 1986
Published in Issue Year 1986 Volume: 105-106 Issue: 105-106

Cite

APA Aydal, D. (1986). DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE. Bulletin of the Mineral Research and Exploration, 105-106(105-106), 106-133.
AMA Aydal D. DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE. Bull.Min.Res.Exp. October 1986;105-106(105-106):106-133.
Chicago Aydal, Doğan. “DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE”. Bulletin of the Mineral Research and Exploration 105-106, no. 105-106 (October 1986): 106-33.
EndNote Aydal D (October 1, 1986) DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE. Bulletin of the Mineral Research and Exploration 105-106 105-106 106–133.
IEEE D. Aydal, “DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE”, Bull.Min.Res.Exp., vol. 105-106, no. 105-106, pp. 106–133, 1986.
ISNAD Aydal, Doğan. “DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE”. Bulletin of the Mineral Research and Exploration 105-106/105-106 (October 1986), 106-133.
JAMA Aydal D. DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE. Bull.Min.Res.Exp. 1986;105-106:106–133.
MLA Aydal, Doğan. “DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE”. Bulletin of the Mineral Research and Exploration, vol. 105-106, no. 105-106, 1986, pp. 106-33.
Vancouver Aydal D. DETERMINING TWO DIMENSIONS OF A CONCEALED CHROMITE ORE BY MICROCOMPUTER MODELLING OF MAGNETIC TOTAL FIELD INTENSITY PROFILE. Bull.Min.Res.Exp. 1986;105-106(105-106):106-33.

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