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Tytuł artykułu

On application of fractal magnetization in Curie depth estimation from magnetic anomalies

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
As an independent geothermal proxy, the Curie-point depth has important geodynamic implications, but its estimation from magnetic anomalies requires an understanding of the spatial correlation of source magnetization, mathematically characterized by a fractal exponent. In this paper, we show that fractal exponent and Curie depth are so strongly inter-connected that attempts to simultaneous or iterative estimation of both of them often turn out to be futile. In cases of true large Curie depths, the iterative “de-fractal” method has a tendency of overcorrecting fractal exponents and thereby producing erroneously small Curie depths and smearing out true geological trends. While true fractal exponent can no way be constant over a large area, a regionally fxed fractal exponent is better than any mathematical treatments that are beyond the limit of data resolution and the underlying physics.
Czasopismo
Rocznik
Strony
1319--1327
Opis fizyczny
Bibliogr. 35 poz.
Twórcy
autor
  • Department of Marine Sciences, Zhejiang University, Zhoushan 316021, China
  • Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
autor
  • Department of Marine Sciences, Zhejiang University, Zhoushan 316021, China
autor
  • Key Laboratory of Crustal Dynamics, Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
Bibliografia
  • 1. Audet P, Gosselin JM (2019) Curie depth estimation from magnetic anomaly data: a re-assessment using multitaper spectral analysis and Bayesian inference. Geophys J Int 218:494–507. https://doi.org/10.1093/gji/ggz166
  • 2. Bansal AR, Gabriel G, Dimri VP, Krawczyk CM (2011) Estimation of depth to the bottom of magnetic sources by a modified centroid method for fractal distribution of sources: an application to aeromagnetic data in Germany. Geophysics 76:L11–L22. https://doi.org/10.1190/1.3560017
  • 3. Blakely RJ (1995) Potential theory in gravity and magnetic applications. Cambridge University Press, Cambridge, pp 1–464
  • 4. Bouligand C, Glen JMG, Blakely RJ (2009J) Mapping Curie temperature depth in the western United States with a fractal model for crustal magnetization. J Geophys Res 114:B11104. https://doi.org/10.1029/2009JB006494
  • 5. Briggs IC (1974) Machine contouring using minimum curvature. Geophysics 9:39–48
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  • 8. Friedman SA, Feinberg JM, Ferré EC, Demory F, Martín-Hernández F, Conder JA, Rochette P (2014) Craton vs. rift uppermost mantle contributions to magnetic anomalies in the United States interior. Tectonophysics 624–625:15–23
  • 9. Gaudreau É, Audet P, Schneider DA (2019) Mapping Curie depth across western Canada from a wavelet analysis of magnetic anomaly data. J Geophys Res 124:4365–4385. https://doi.org/10.1029/2018JB016726
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  • 12. Li C-F, Wang J (2018) Thermal structures of the Pacific lithosphere from magnetic anomaly inversion. Earth Planet Phys 2:52–66
  • 13. Li C-F, Chen B, Zhou Z (2009) Deep crustal structures of eastern China and adjacent seas revealed by magnetic data. Sci China Ser D Earth Sci 52:984–993. https://doi.org/10.1007/s11430-009-0096-x
  • 14. Li C-F, Shi XB, Zhou ZY, Li JB, Geng JH, Chen B (2010) Depths to the magnetic layer bottom in the South China Sea area and their tectonic implications. Geophys J Int 182:1229–1247. https://doi.org/10.1111/j.1365-246X.2010.04702.x
  • 15. Li C-F, Wang J, Lin J, Wang T (2013G) Thermal evolution of the North Atlantic lithosphere: new constraints from magnetic anomaly inversion with a fractal magnetization model. Geochem Geophys Geosyst 14:5078–5105. https://doi.org/10.1002/2013GC004896
  • 16. Li C-F, Lu Y, Wang J (2017) A global reference model of Curie-point depths based on EMAG2. Sci Rep 7:45129. https://doi.org/10.1038/srep45129
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  • 20. Maus S, Barckhausen U, Berkenbosch H, Bournas N, Brozena J, Childers V, Dostaler F, Fairhead JD, Finn C, von Frese RRB, Gaina C, Golynsky S, Kucks R, Luhr H, Milligan P, Mogren S, Müller D, Olesen O, Pilkington M, Saltus R, Schreckenberger B, Thébault E, Caratori Tontini F (2009G) EMAG2: a 2-arc-minute resolution earth magnetic anomaly grid compiled from satellite, airborne and marine magnetic measurements. Geochem Geophys Geosyst 10:Q08005. https://doi.org/10.1029/2009GC002471
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  • 23. O’Reilly W (1984) Rock and mineral magnetism. Blackie Academy and Professor, London
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  • 27. Salem A, Green C, Ravat D, Singh KH, East P, Fairhead JD, Mogren S, Biegert E (2014) Depth to Curie temperature across the central Red Sea from magnetic data using the de-fractal method. Tectonophysics 624–625:75–86
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Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-7e073379-ec60-47c1-92ac-48ff8a2d4ca8
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