Comparison of the Third- order moving average and least square methods for estimating of shape and depth residual magnetic anomalies
Subject Areas :
Mineralogy
Mohammad Fouladi
1
,
Mirsattar Meshinchi Asl
2
,
Mahmoud Mehramuz
3
,
Nima Nezafati
4
1 - Department of Earth Sciences, Science and Research Branch, Islamic Azad University, Tehran, Iran
2 - Department of Earth Sciences, Science and Research Branch, Islamic Azad University, Tehran, Iran
3 - Department of Earth Sciences, Science and Research Branch, Islamic Azad University, Tehran, Iran
4 - Department of Earth Sciences, Science and Research Branch, Islamic Azad University, Tehran, Iran
Received: 2020-06-30
Accepted : 2021-05-05
Published : 2021-07-01
Keywords:
References:
Abdelrahman EM, Abo-Ezz ER (2001) Higher derivatives analysis of 2-D magnetic data, Geophysics 66: 205–212.
Abdelrahman EM, Abo-Ezz ER, Essa KS, El-Araby TM, Soliman KS (2007) A new least-squares minimization approach to depth and shape determination from magnetic data, Geophysical Prospecting 55: 433–446.
Abdelrahman EM, Essa KS (2015) A new method for depth and shape determinations from magnetic data, Pure and Applied Geophysics 172: 439–460.
Abdelrahman EM, Essa KS, El-Araby TM, Abo-Ezz ER (2016) Depth and shape solutions from second moving average residual magnetic anomalies, Exploration Geophysics 43: 178–189.
Atchuta Rao DA, Ram Babu HV (1980) Properties of the relation figures between the total, vertical, and horizontal field magnetic anomalies over a long horizontal cylinder ore body, Current Science 49: 584–585.
Essa KS, Elhussein M (2018) PSO (Particle Swarm Optimization) for Interpretation of Magnetic Anomalies Caused by Simple Geometrical Structures, Pure and Applied Geophysics 175(2).
Essa KS, Elhussein M (2019) Interpretation of Magnetic Data Through Particle Swarm Optimization: Mineral Exploration Cases Studies, Natural Resources Research 29: 521-537.
Gay P (1963) Standard curves for interpretation of magnetic anomalies over long tabular bodies, Geophysics, 28: 161–200.
Gay P (1965) Standard curves for interpretation of magnetic anomalies over long horizontal cylinders, Geophysics 30: 818–828.
Hartman RR, Teskey DJ, Friedberg JL (1971) A system for rapid digital aeromagnetic interpretation, Geophysics 36: 891–918.
Hinze WJ (1990) The role of gravity and magnetic methods in engineering and environmental studies, Geotechnical and Environmental Geophysics 75–126.
Jain S (1976) An automatic method of direct interpretation of magnetic profiles, Geophysics 41: 531–541.
McGrath PH, Hood PJ (1970) The dipping dike case: A computer curve-matching method of magnetic interpretation, Geophysics 35:831–848.
Paul PA (1964) Depth rules for some geometric bodies for interpretation of aeromagnetic anomalies, Geophysics Research Bulletin 2:15–21.
Pengfei L, Tianyou L, Peimin Z, Yushan Y, Qiaoli Z, Henglei Z, Guoxiong C (2017) Depth Estimation for Magnetic/Gravity Anomaly Using Model Correction, Pure and Applied Geophysics 174: 1729–1742.
Prakasa Rao TKS, Subrahmanyan M, Srikrishna Murthy A (1986) Nomograms for the direct interpretation of magnetic anomalies due to long horizontal cylinders, Geophysics 51: 2156–2159.
Prakasa Rao TKS, Subrahmanyan M (1988) Characteristic curves for inversion of magnetic anomalies of spherical ore bodies, Pure and Applied Geophysics 126: 69–83.
Radhakrishna Murthy IV (1967) Note on the interpretation of magnetic anomalies of spheres, I. G. U. 4: 41–42.
Reid AB, Allsop JM, Granser H, Millett AJ, Somerton IW (1990) Magnetic interpretation in three dimensional using Euler deconvolution, Geophysics 55: 80–91.
Stanley JM (1977) Simplified magnetic interpretation of the geologic contact and thin dike, Geophysics 42: 1236–1240.
Steenland NC, Slack HA, Lynch VM, Langan L (1968) Discussion on The geomagnetic gradiometer, Geophysics 32: 877– 892.
Thompson DT (1982) EULDPH a new technique for making computer-assisted depth estimates from magnetic data, Geophysics 47: 31–37.
Werner S (1953) Interpretation of Magnetic Anomalies of Sheet-like Bodies, Sveriges Geologiska Underok Series C 43: N6.