Abstract
Marine magnetic anomalies are continuous records of the history of geomagnetic field reversals preserved in oceanic crust over the past ~160 Myr. In addition, the shape of the magnetic anomalies depends on the effective inclinations of the external magnetic field vector \(I_{0}^{'}\) and the remanent magnetization vector \(I_{r}^{'}\) can be numerically expressed by the skewness parameter \(\theta = I_{r}^{'} + I_{0}^{'} - \pi\). By determining the values of theta from magnetic profiles the inclination of the remanent magnetization can be found which leads to estimates of the contribution of the averaged non-dipole field. We investigated a series of closely spaced magnetic profiles intersecting the axis of the Carlsberg Ridge near the equator, and intersecting the axial anomaly region (Brunhes normal polarity chron C1n) and adjacent anomalies (subchron C2, Matuyama chron). The observed inclination anomaly near the equator can be viewed as an evidence of presence of the quadrupole component in the averaged non-dipole field.
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References
Acton, G.D., Petronotis, K.E., Cape, C.D., Ilg, S.R., Gordon, R.G., Bryan, P.C.: A test of the geocentric axial dipole hypothesis from an analysis of the skewness of the central marine magnetic anomaly. Earth Planet Sci. Lett. 144, 337–346 (1996)
Ben’kova, N.P., Khramov, A.N., Cherevko, T.N., Adam, N.V.: Spherical harmonic analysis of the paleomagnetic field. Earth Planet. Sci. Lett. 18, 141–147 (1973)
Cox, A.: The frequency of geomagnetic reversals and the symmetry of the non dipole field. Rev. Geophys. 13(3), 35–51 (1975)
DeMets, C., Gordon, R.G., Argus, D.F.: Geologically current plate motions. Geophys. J. Int. 181(1), 1–80 (2010)
Gay, S.P.: Standard curves for interpretation of magnetic anomalies over long tabular bodies. Geophysics 28, 161–200 (1963)
International Association of Geomagnetism and Aeronomy (IAGA): Division V, Working group 8, international geomagnetic reference field 2000. Geophys. J. Int. 141, 259–262 (2000)
Ivanov, S.A., Merkuryev, S.A.: Some remarks on resolving and interpretation of short wavelength marine magnetic anomalies. In: Proceedings of the 11th International School and Conference “Problems of Geocosmos”, SPb.: VVM Publishing, pp. 37–44 (2016)
Ivanov, S.A., Merkuriev, S.A.: Preliminary results of the Geohistorical and Paleomagnetic analysis of marine magnetic anomalies in the northwestern Indian Ocean. In: Nurgaliev, D. et al. (eds.) Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism. International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism (Kazan, Russia), pp. 479–490. Springer International Publishing (2019)
Langel, R.A., Estes, R.H.: A geomagnetic field spectrum. Geophys. Res. Lett. 9, 250–253 (1982)
Macmillan, S., Maus, S.: International geomagnetic reference field-the tenth generation. Earth Planets Space 57, 1135–1140 (2015)
Merkouriev, S.A., Sotchevanova, N.A.: Structure and evolution of the Carlsberg Ridge: evidence for nonstationary spreading on old and modern spreading centers. Current Sci. 85, 334–338 (2003)
Merkouriev, S., DeMets, C.: Constraints on Indian plate motion since 20 Ma from dense Russian magnetic data: implications for Indian plate dynamics. Geochem. Geophys. Geosyst. 7, Q02002 (2006). https://doi.org/10.1029/2005gc001079
Merrill, R.T., McElhinny, M.W.: Anomalies in the time averaged paleomagnetic field and their implications for the lower mantle. Rev. Geophys. Space Phys. 15, 309–323 (1977)
Merrill, R.T., McElhinny, M.W., McFadden, P.L.: The Magnetic Field of the Earth, p. 531. Academic Press, New York (1996)
Opdyke, N.D.: Paleomagnetism of deep-sea cores. Rev. Geophys. 10(1), 213–249 (1972)
Roest, W.R., Arkani-Hamed, J., Verhoef, J.: The seafloor spreading rate dependence of the anomalous skewness of marine magnetic anomalies. Geophys. J. Int. 109(3), 653–669 (1992)
Schneider, D.A.: An estimate of the long-term non-dipole field from marine magnetic anomalies. Geophys. Res. Lett. 15, 1105–1108 (1988)
Schneider, D.A., Kent, D.V.: Inclination anomalies from Indian Ocean sediments and the possibility of a standing nondipole field. J. Geophys. Res. 93(B10), 11621–11630 (1988)
Schneider, D.A., Kent, D.V.: The time-averaged paleomagnetic field. Rev. Geophys. 28(1), 71–96 (1990)
Schouten, H.: A fundamental analysis of magnetic anomalies over oceanic ridges. Mar. Geophys. Res. 1(2), 111–144 (1971)
Schouten, H., McCamy, K.: Filtering marine magnetic anomalies. J. Geophys. Res. 77, 7089–7099 (1972)
Schouten, H., Cande, S.C.: Palaeomagnetic poles from marine magnetic anomalies. Geophys. J. R. Astron. Soc. 44, 567–575 (1976)
Wessel, P., Smith, W.H.F.: Free software helps map and display data. Eos Trans. AGU 72, 441–446 (1991)
Acknowledgements
In preparing the plots, the GMT program package [23] was used. We are grateful to Dr. Karl Fabian and Dr. Andrei Kosterov for critically reading the manuscript and constructive reviews.
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Merkuriev, S.A., Demina, I.M., Ivanov, S.A. (2020). Preliminary Estimation of the Non-dipole Part of the Geomagnetic Field in the Quaternary Period Based on the Investigation of Marine Magnetic Anomalies on the Carlsberg Ridge. In: Yanovskaya, T., Kosterov, A., Bobrov, N., Divin, A., Saraev, A., Zolotova, N. (eds) Problems of Geocosmos–2018. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-21788-4_13
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