Fusion of Ground and Airborne Magnetic Data Using Multi-Layer Equivalent Source Method

被引:0
作者
Gao B. [1 ,2 ]
Hu Z. [1 ]
Li D. [1 ]
Du J. [1 ,3 ]
机构
[1] Hubei Subsurface Multi-Scale Imaging Key Laboratory, Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan
[2] Institute of Geological Survey, Central South Bureau of China Metallurgical Geology Bureau, Wuhan
[3] State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan
来源
Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences | 2021年 / 46卷 / 05期
关键词
Data fusion; Data transformation; Extension; Geophysics; Interpolation; Multi-layer equivalent source;
D O I
10.3799/dqkx.2020.134
中图分类号
学科分类号
摘要
With the accumulation of measured magnetic data, it is becoming urgent to use these data efficiently. Previous studies have shown that it is difficult to meet the accuracy requirement for solving geological problems by using the measured data from a single observation method. Because of the limitations and differences in resolution, accuracy, elevation and range of magnetic data obtained by various methods, single dataset can only effectively reflect the information over a certain range of wavelength of magnetic field. An effective way to solve this problem is the fusion of data. Therefore, based on the equivalent source method, a multi-layer equivalent source technology is proposed in this paper, which can be applied to the fusion of ground and airborne magnetic data to improve the accuracy of interpolation, continuation, extension, transformation, et al. According to the spectral characteristics of observation data, three-layer equivalent sources at different depths are used to fit the measured data. Compared with the traditional single-layer equivalent source method, it can reduce the blindness for setting equivalent sources, and improve the ordering and structural performance for allotting observation information into equivalent sources. Synthetic experiment shows that the three-layer model has higher computational accuracy, and data fusion can significantly improve each dataset. Finally, the method is applied to the fusion of ground and airborne magnetic data in Jinniu basin, Hubei, and abundant magnetic data with regular distribution on a plane are obtained. © 2021, Editorial Department of Earth Science. All right reserved.
引用
收藏
页码:1881 / 1895
页数:14
相关论文
共 40 条
  • [1] An Y.L., Chai Y.P., Zhang M.H., Et al., An Optimal Model of the Equivalent Source for Reduction-to-Plane of Potential Field on Uneven Surface and the New Method to Deduce Unit Potential Field Expression of the Optimal Model, Chinese Journal of Geophysics, 56, 7, pp. 2473-2483, (2013)
  • [2] Andrews S. B., Moore P., King M. A., Mass Change from GRACE: A Simulated Comparison of Level-1B Analysis Techniques, Geophysical Journal International, 200, 1, pp. 503-518, (2015)
  • [3] Asgharzadeh M. F., von Frese R. R. B., Kim H. R., Spherical Prism Magnetic Effects by Gauss- Legendre Quadrature Integration, Geophysical Journal International, 173, 1, pp. 315-333, (2008)
  • [4] Barnes G., Lumley J., Processing Gravity Gradient Data, Geophysics, 76, 2, pp. I33-I47, (2011)
  • [5] Barzaghi R., Tselfes N., Tziavos I. N., Et al., Geoid and High Resolution Sea Surface Topography Modelling in the Mediterranean from Gravimetry, Altimetry and GOCE Data: Evaluation by Simulation, Journal of Geodesy, 83, 8, pp. 751-772, (2008)
  • [6] Bhattacharyya B.K., Chan K.C., Reduction of Magnetic and Gravity Data on an Arbitrary Surface Acquired a Region of High Topographic, Geophysics, 42, 42, pp. 1411-1430, (1977)
  • [7] Clark D.A., New Method for Interpretation of Magnetic Vector and Gradient Tensor Data Ⅱ: Application to the Mount Leyshon Anomaly, Queensland, Australia, Exploration Geophysics, 44, 2, pp. 114-127, (2013)
  • [8] Cordell L., Grauch V.J.S., Reconciliation of the Discrete and Integral Fourier Transforms, Geophysics, 47, 2, pp. 237-243, (1982)
  • [9] Dampney C. N. G., The Equivalent Source Technique, Geophysics, 34, 1, pp. 39-53, (1969)
  • [10] Du J.S., Chen C., Progress and Outlook in Global Lithospheric Magnetic Field Modelling by Satellite Magnetic Measurements, Progress in Geophysics, 30, 3, pp. 1017-1033, (2015)