Abstract
Thermomagnetic and microprobe analyses are carried out and a set of magnetic characteristics are measured for 25 meteorites and 3 tektites from the collections of the Vernadsky Geological Museum of the Russian Academy of Sciences and Museum of Natural History of the North-East Interdisciplinary Science Research Institute, Far Eastern Branch of the Russian Academy of Sciences. It is found that, notwithstanding their type, all the meteorites contain the same magnetic minerals and only differ by concentrations of these minerals. Kamacite with less than 10% nickel is the main magnetic mineral in the studied samples. Pure iron, taenite, and schreibersite are less frequent; nickel, various iron spinels, Fe-Al alloys, etc., are very rare. These minerals are normally absent in the crusts of the Earth and other planets. The studied meteorites are more likely parts of the cores and lower mantles of the meteoritic parent bodies (the planets). Uniformity in the magnetic properties of the meteorites and the types of their thermomagnetic (MT) curves is violated by secondary alterations of the meteorites in the terrestrial environment. The sediments demonstrate the same monotony as the meteorites: kamacite is likely the only extraterrestrial magnetic mineral, which is abundant in sediments and associated with cosmic dust. The compositional similarity of kamacite in iron meteorites and in cosmic dust is due to their common source; the degree of fragmentation of the material of the parent body is the only difference.
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Baker, J., Bizzarro, M., Witting, N., Connelly, J., and Haack, H., Early Planetesimal Melting from an Age 4.566 Gyr for Differentiated Meteorites, Nature, 2005, vol. 436, no. 7054, pp. 1127–1131.
Bonvier, A. and Wadhwa, M., The Age of the Solar System Redefined by the Oldest Pb-Pb Age of Meteoritic Inclusion, Nat. Geosci., 2010, vol. 3, pp. 637–641.
Bozorth, R., Ferromagnetism, Princeton, New Jersey: Van Nostrand, 1951.
Cassiamani, G., Kayzre, J.D., Ferro, R., Klotz, U.E., Locaze, J., and Wollants, P., Critical Evaluation of the Fe-Ni, Fe-Ti, and Fe-Ni-Ti Alloy Systems, Intermetallic, 2006, vol. 14, pp. 1312–1325.
Encyclopedia Britannica, Meteorites, Second edition. http://www.eb.com.
Frondel, J.W., Lunar Mineralogy, Cambridge, MA: Harvard University Press, 1975.
Gambino, R.J., McGuire, T.R., and Nakamura, Y. Magnetic Properties of the Iron-Group Metal Phosphides, J. Appl. Phys., 1967, vol. 38, no. 3, pp. 1253–1255.
Grachev, A.F., Kollmann, H.A., Korchagin, O.A., et al., The K/T boundary of Gams (Eastern Alps, Austria) and the Nature of Terminal Cretaceous Mass Extinction, Grachev, A.F., Ed., Abh. Geol. Bundesans. (Austria), 2009, vol. 63, pp. 89–134.
Gus’kova, E.G., Magnitnye svoistva meteoritov (Magnetic Properties of Meteorites), Leningrad: Nauka, 1972.
Hubbard, W., Planetary Interiors, New York: Van Nostrand Reinhold, 1984.
Kohout, T., Physical Properties of Meteorites and Their Role in Planetology, Rep. Ser. Geophys., 2009, no. 60, pp. 3–51.
Marakushev, A.A., Granovskii, L.B., Zinov’eva, N.G., and Mitreikina, O.B., Kosmicheskaya petrologiya (Space Petrology), Moscow: MGU, 1992.
McFadden, L., Weissman, P.R., and Johnson, T.V., Encyclopedia of the Solar System, San Diego: Academic Press, 2007. Meteoritical Bulletin, 2000, no. 84-2010, no. 98.
Meyer, A.J.P. and Cadevill, M.C., Magnetic Properties of the Fe-Ni Phosphides, Proc. Int. Conf. Mag. Cryst., 1961, Supplement B-1 to J. Phys. Soc. Japan, 1962, vol. 17, pp. 223–225.
Nagata, T., Rock Magnetism, Tokyo: Maruzen, 1961.
Nagata, T., Funaki, M. and J. Danon, Magnetic Properties of Tetrataenite-Rich Iron Meteorites, Mem. Natl. Inst. Polar Res., Spec. Issue, 1986, vol. 41, pp. 364–370.
Nagata, T., Danon, J., and Funaki, M., Magnetic Properties of Ni-Rich Iron Meteorites, Mem. Natl. Inst. Polar Res., Spec. Issue, 1987, vol. 46, pp. 263–282.
Patterson, C., Age of Meteorites and the Earth, Geochim. Cosmochim. Acta, 1956, vol. 10, pp. 230–237.
Pechersky, D.M., Bagin, V.I., Brodskaya, S.Yu., and Sharonova, Z.V., Magnetizm i usloviya obrazovaniya izverzhennykh gornykh porod (Magnetism and Formation Conditions of Igneous Rocks), Leningrad: Nauka, 1975.
Pechersky, D.M. and Didenko, A.N., Paleoaziatskii okean: petromagnitnaya i paleomagnitnaya informatsiya o ego litosfere (Paleo-Asian Ocean: Rock Magnetic and Paleomagnetic Information on Its Lithosphere), Moscow: OIFZ RAN, 1995.
Pechersky, D.M., Nourgaliev, D.K., and Trubikhin, V.M., Native Iron in Miocene Sediments, Rus. J. Earth Sci., 2008, vol. 10, ES6004. doi: 10.2205/2008ES000306
Pechersky, D.M., Metallic Iron and Nickel in Cretaceous and Cenozoic Sediments: the Results of Thermomagnetic Analysis, J. Environ. Prot., 2010, vol. 1, no. 2, pp. 143–154.
Pechersky, D.M., Nurgaliev, D.K., Fomin, V.A., Sharonova, Z.V., and Gil’manova, D.M., Extraterrestrial Iron in the Cretaceous-Danian Sediments, Izv. Phys. Earth, 2011b, vol. 47, no. 5, pp. 379–401.
Pechersky, D.M. and Sharonova, Z.V., Thermomagnetic Evidence of Native Iron in Sediments, Izv. Phys. Earth, 2012, vol. 48, no. 4, pp. 320–325.
Petromagnitnaya model’ litosfery (Petromagnetic Model of Lithosphere), Pashkevich, I.K. and Pecherskii, D.M., Eds., Kiev: Naukova Dumka, 1994.
Rochette, P., Weiss, B.P., and Gattacceca, J., Magnetism of Extraterrestrial Materials, Elements, 2009, vol. 5, pp. 223–228.
Sugiura, N. and Strangway, D.W., The Magnetic Properties of the Abee Meteorite: Evidence for a Strong Magnetic Field in the Early Solar System, Proc. Lunar Planet. Sci., 1981, vol. 128, pp. 1243–1256.
Sugiura, N. and Strangway, D.W., Magnetic Studies of Meteorites, in Meteorites and the Early Solar System II, Lauretta D.S. and McSween, H.Y., Eds., Arizona: Univ. Arizona Press, 1987, pp.595–615. Supplement, http://paleomag.ifz.ru/books/2012-pechersky-et-al-meteorite-data-supplement.rar
Terho, M., Pesonen, L.J., Kukkonen, I.T., and Bukovanska, M., The Petrophysical Classification of Meteorites, Stud. Geophys. Geod., 1993, vol. 37, pp. 65–82.
Uehara, M. and Naramura, N., Experimental Constraints on Magnetic Stability of Chondrites and Paleomagnetic Significance of Dusty Olivines, Earth Planet. Sci. Lett., 2006, vol. 250, pp. 292–305.
Wasilewski, P., Magnetic Characterization of the New Magnetic Mineral Tetrataenite and Its Contrast with Isochemical Taenite, Phys. Earth Planet. Inter., 1988, vol. 52, pp. 150–158.
Weiss, B.P., Gattacceca, J., Stanley, S., Rochette, P., and Christensen, U.R., Paleomagnetic Records of Meteorites and Early Planetesimal Differentiation, Space Sci. Rev., 2010, vol. 154, nos. 1–4, pp. 341–390. doi: 10.1007/s11214009-9580-z
Zharkov, V.N., Vnutrennee stroenie Zemli i planet (Internal Structure of Earth and Planets), Moscow: Nauka, 1983.
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Original Russian Text © D.M. Pechersky, G.P. Markov, V.A. Tsel’movich, Z.V. Sharonova, 2012, published in Fizika Zemli, 2012, Nos. 7–8, pp. 103–120.
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Pechersky, D.M., Markov, G.P., Tsel’movich, V.A. et al. Extraterrestrial magnetic minerals. Izv., Phys. Solid Earth 48, 653–669 (2012). https://doi.org/10.1134/S1069351312070051
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DOI: https://doi.org/10.1134/S1069351312070051