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Enjoy the experiences below on your mobile device, or visit this page on Mac or PC for even more ways to explore. Eyes on the Earth. Magnetic exploration models incorporating remanence, demagnetization and anisotropy: HP 41C handheld computer algorithms , Explor.

Fedi M. On the interpretation of magnetic anomalies for strong remanent magnetizations , Pure appl. A method to estimate the total magnetization direction from a distortion analysis of magnetic anomalies , Geophys.

Gao B. Application of aero-surface and boreholemagnetic explorat ion to the prospect ing of exhausted mines in the Daye iron mine , Geol.

Gerovska D. Estimating the magnetization direction of sources from southeast Bulgaria through correlation between reduced-to-the-pole and total magnitude anomalies , Geophys.

Guo L. Three-dimensional correlation imaging for total amplitude magnetic anomaly and normalized source strength in the presence of strong remanent magnetization , J. Guo W. Systematic error analysis of demagnetization and implications for magnetic interpretation , Geophysics , 66 , — Self demagnetisation corrections in magnetic modelling: some examples , Explor.

Krahenbuhl R. Investigation of magnetic inversion methods in highly magnetic environments under strong self-demagnetization effect , Geophysics , 82 , J83 — J Magnetic forward modelling and inversion for high susceptibility , Geophys. A 3D total magnetization inversion applicable when significant, complicated remanence is present , Geophysics , 74 , L21 — L An approach for estimating the magnetization direction of magnetic anomalies , J.

Late Mesozoic magmatism from the Daye region, eastern China: U—Pb ages, petrogenesis, and geodynamic implications , Contributions to Mineralogy and Petrology , , — Inversion of magnetic anomaly on rugged observation surface in the presence of strong remanent magnetization , Geophysics , 79 , J11 — J Comprehensive approaches to 3D inversion of magnetic data affected by remanent magnetization , Geophysics , 75 , L1 — L Liu S. Okiwelu A.

Inversion of borehole magnetic data for prospecting deep-buried minerals in areas with near-surface magnetic distortions: a case study from the Daye iron-ore deposit in Hubei, central China , Near Surf. Magnetization vector imaging for borehole magnetic data based on magnitude magnetic anomaly , Geophysics , 78 , D — D Naidu P. Phillips J. Can we estimate total magnetization directions from aeromagnetic data using Helbig's integrals? Earth Planets Space , 57 , — Pilkington M. Mitigating remanent magnetization effects in magnetic data using the normalized source strength , Geophysics , 78 , J25 — J Sharma P.

Demagnetization effect of a rectangular prism , Geophysics , 33 , — Shearer S. Stoner E. The demagnetizing factors for ellipsoids , Lond. Sun J. Assessing the uncertainty of magnetization directions from clustering inversion and its effect on geology differentiation , in Proceedings of the 87th SEG Annual Meeting Expanded Abstracts , pp.

Wang M. Magnetization vector inversion equations and 2D forward and inversed model study , Chin. Revised apparent polar wander path of the Yangtze Block and its tectonic implications , Sci.

China Ser. D: Earth Sci. Yang Y. Interactive 3D forward modeling of total field surface and three-component borehole magnetic data for the Daye iron-ore deposit Central China , J. Yuan X. Error analysis of calculation of total field anomaly due to highly magnetic bodies , Chin. Zhou J. Three-dimensional cross-gradient joint inversion of gravity and normalized magnetic source strength data in the presence of remanent magnetization , J.

Zhu R. Paleomagnetic constraints on the tectonic history of the major blocks of China duing the Phanerozoic , Sci. Oxford University Press is a department of the University of Oxford. It furthers the University's objective of excellence in research, scholarship, and education by publishing worldwide.

Sign In or Create an Account. Sign In. Advanced Search. Search Menu. Article Navigation. Close mobile search navigation Article Navigation. Volume Three-dimensional inversion of magnetic data in the simultaneous presence of significant remanent magnetization and self-demagnetization: example from Daye iron-ore deposit, Hubei province, China.

Shuang Liu , Shuang Liu. Oxford Academic. Maurizio Fedi. Xiangyun Hu. E-mail: xyhu cug. Yang Ou. Jamaledin Baniamerian. Boxin Zuo. Yuegao Liu. Rixiang Zhu. Revision received:. Select Format Select format. Permissions Icon Permissions.

SUMMARY Natural remanent magnetization and self-demagnetization on high-susceptibility bodies are two important factors affecting magnetic data inversion. Magnetic anomalies , modelling and interpretation , Rock and mineral magnetism , Inverse theory.

In this study, the magnetization vector is determined by sequentially estimating the total magnetization direction and recovering the magnetization intensity. By this approach, we estimate the inclination and declination of the total magnetization vector based on the minimal values of the reduced-to-pole RTP fields obtained by assuming various magnetization directions.

Next, the inversion of the total magnetization intensity is performed based on the estimated inclination and declination. For this purpose, the subsurface is divided into cubic cells, assuming that each cell has a homogeneous total magnetization vector. For low-susceptibility bodies, the total magnetization M is equal to the vector sum of induced magnetization M i and remanent magnetization M r Fig. Open in new tab Download slide. When the self-demagnetization effect is not negligible e.

If we assume that the self-demagnetization only affects the intensity of magnetization and it does not change their directions, the self-demagnetization problem would be greatly simplified Fig.

For high-susceptibility magnetic sources, the apparent susceptibility in eq. Table 1. Sharma Stoner Open in new tab. Table 2. Rocks and ores. Magnetite 0. Table 3. Sampling positions. Number of samples. Final Q. TMK Line48—50 stope 7 1. Estimating source location using normalized magnetic source strength calculated from magnetic gradient tensor data. Google Scholar Crossref. Search ADS. An enhanced method for estimation of body magnetization direction from pseudogravity and gravity data.

New methods for interpretation of magnetic vector and gradient tensor data I: eigenvector analysis and the normalised source strength. Methods for determining remanent and total magnetisations of magnetic sources—a review. Notes on rock magnetization characteristics in applied geophysical studies. Investigation of magnetization and density of a north Atlantic seamount using Poisson's theorem.

Magnetic exploration models incorporating remanence, demagnetization and anisotropy: HP 41C handheld computer algorithms. On the interpretation of magnetic anomalies for strong remanent magnetizations. A method to estimate the total magnetization direction from a distortion analysis of magnetic anomalies.

Application of aero-surface and boreholemagnetic explorat ion to the prospect ing of exhausted mines in the Daye iron mine.

Estimating the magnetization direction of sources from southeast Bulgaria through correlation between reduced-to-the-pole and total magnitude anomalies. Three-dimensional correlation imaging for total amplitude magnetic anomaly and normalized source strength in the presence of strong remanent magnetization.

Systematic error analysis of demagnetization and implications for magnetic interpretation. Investigation of magnetic inversion methods in highly magnetic environments under strong self-demagnetization effect.

A 3D total magnetization inversion applicable when significant, complicated remanence is present. An approach for estimating the magnetization direction of magnetic anomalies. Late Mesozoic magmatism from the Daye region, eastern China: U—Pb ages, petrogenesis, and geodynamic implications. Inversion of magnetic anomaly on rugged observation surface in the presence of strong remanent magnetization.

Comprehensive approaches to 3D inversion of magnetic data affected by remanent magnetization. Total magnetization vector inversion using guided fuzzy c-means clustering. Inversion of borehole magnetic data for prospecting deep-buried minerals in areas with near-surface magnetic distortions: a case study from the Daye iron-ore deposit in Hubei, central China.

Magnetization vector imaging for borehole magnetic data based on magnitude magnetic anomaly.