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Campo del Cielo – an Iron Meteorite found in Argentina

  • R. Haubner

    Roland Haubner is Ao.Univ.Prof. at TU-Wien. His fields of activity till now were industrial tungsten production, CVD (Chemical Vapor Deposition) and the low-pressure diamond deposition. He is also involved in materials characterization, ceramics, corrosion and archaeometallurgy.

    and S. Strobl

    Susanne Strobl is working as a scientific officer at the Institute of Chemical Technologies and Analytics (TU-Wien) and is teaching supervisor of metallography. She studied chemistry and her doctoral thesis was about sintered steels.

Published/Copyright: September 11, 2021
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Abstract

Fragments of the “Campo del Cielo” meteorite were first reported by conquistadores in Argentina in as early as 1576. This meteorite belongs to the group of iron meteorites and is classified as a group IA coarse octahedrite. The use of meteoric iron to make objects of daily use or hunting weapons in prehistoric times is only confirmed by very few finds. Metallographic examinations were performed to assess if it was realistic and in fact feasible to process meteoric iron.

The bulk of the examined “Campo del Cielo” meteorite fragment found in Argentina is kamacite (α-Fe) with approx. 5.3 wt.% of dissolved Ni. Graphite was also detected in addition to various non-metallic phases. Due to high temperatures during processing, graphite can dissolve and a steel microstructure would form as a result.

Kurzfassung

Teile des Meteoriten „Campo del Cielo“ wurden bereits 1576 von Konquistadores in Argentinien beschrieben. Dieser Meteorit gehört zu den Eisenmeteoriten und wird als grober Oktaedrit der Gruppe IA klassifiziert. Die Nutzung von Meteoriteneisen für Gebrauchsgegenstände oder Jagdwaffen in prähistorischer Zeit ist nur durch wenige Fundstücke belegt. Durch die metallographischen Untersuchungen sollte abgeschätzt werden, ob eine Verarbeitung von Meteoriteneisen realistisch durchzuführen war.

Das untersuchte Teilstück des Meteorits „Campo del Cielo“ aus Argentinien enthielt als Hauptmasse Kamacit (α-Fe) mit etwa 5,3 Gew.-% gelöstem Ni. Neben diversen nichtmetallischen Phasen wurde auch Graphit nachgewiesen. Durch hohe Temperaturen bei der Verarbeitung kann sich der Graphit auflösen und es würde ein Stahl entstehen.

Schlüsselwörter: Meteorit; Kamacit; Schreibersit; Graphit

About the authors

R. Haubner

Roland Haubner is Ao.Univ.Prof. at TU-Wien. His fields of activity till now were industrial tungsten production, CVD (Chemical Vapor Deposition) and the low-pressure diamond deposition. He is also involved in materials characterization, ceramics, corrosion and archaeometallurgy.

S. Strobl

Susanne Strobl is working as a scientific officer at the Institute of Chemical Technologies and Analytics (TU-Wien) and is teaching supervisor of metallography. She studied chemistry and her doctoral thesis was about sintered steels.

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5 Acknowledgements

The authors would like to thank Mr Nico Neubauer who assisted in the metallographic examinations as part of his bachelor’s thesis and Mr Johannes Zbiral who performed XRF analysis.

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5 Danksagung

Unser Dank geht an Herrn Nico Neubauer, der im Rahmen seiner Bachelorarbeit bei den metallographischen Untersuchungen mitgeholfen hat. Herrn Johannes Zbiral möchten wir für die RFA Messungen danken.

References / Literatur

[1] Comelli, D.; D'Orazio, M.; Folco, L.; El-Halwagy, M.; Frizzi, T.; Alberti, R.; Capogrosso, V.; Elnaggar, A.; Hassan, H.; Nevin, A.; Porcelli, F.; Rashed, M.; Valentini, G.: The meteoritic origin of Tutankhamun's iron dagger blade, Meteoritics & Planetary Science 51 (2016) 1301–1309 DOI: 10.1111/maps.1266410.1111/maps.12664Search in Google Scholar

[2] McCartney, A.P.; Mack Source D.J.: Iron Utilization by Thule Eskimos of Central Canada, American Antiquity 38 (1973) 328–339 DOI: 10.2307/27972010.2307/279720Search in Google Scholar

[3] Cassidy, W.A.; Villar, L.M.; Bunch, T.E.; Kohman, T.P.; Milton, D.J.: Meteorites and craters of Campo del Cielo, Argentina. Science 149 (1965) 1055–1064 DOI: 10.1126/science.149.3688.105510.1126/science.149.3688.1055Search in Google Scholar

[4] Rubín de Celis, M.: Philosophical Transactions of The Royal Society of London 78 (1788) 37–42 DOI: 10.1098/rstl.1788.000410.1098/rstl.1788.0004Search in Google Scholar

[5] Bunch, T.E.; Cassidy, W.A.: Impact-induced deformation in Campo del Cielo meteorite. in: Shock Metamorphism of Natural Materials, (1968) B.M. French, N.M. Short (Eds.), Mono Book Corp., Baltimore, MD, 601–612Search in Google Scholar

[6] Cabanillas, E.D.; Palacios, T.A.: SEM Studies of a Campo del Cielo Meteorite Fall, Microsc Microanal 9 (2003) 632–633 DOI: 10.1017/S143192760344316X10.1017/S143192760344316XSearch in Google Scholar

[7] Axon, H.J.; Smith, P.L.: A metallographie study of some iron meteorites of high nickel content, Mineralogical Magazine38 (1972) 736–755 DOI: 10.1180/minmag.1972.038.298.1010.1180/minmag.1972.038.298.10Search in Google Scholar

[8] Vander Voort G.F.: Metallography of Iron Meteorites, Advanced Materials & Processes 159 (2001) 37–41Search in Google Scholar

[9] Mitt. von Freunden der Naturwissenschaften in Wien IV (1848) 86Search in Google Scholar

[10] Reynolds, M.: Classifications of Meteorites, J. of the Association of Lunar&Planetary Observers, 46 (2004) 13–17Search in Google Scholar

[11] Vander Voort G.F.: A Note on Metallographic Meteorites, Materials Characterization 29 (1992) 223–241 DOI: 10.1016/1044-5803(92)90117-Z10.1016/1044-5803(92)90117-ZSearch in Google Scholar

[12] Strobl, S.; Haubner, R.: Investigation of "Neumann lines" in powder metallurgical samples and meteorites, Acta Metallurgica Slovaca, 13 (2007) 795–801Search in Google Scholar

[13] Hazen, R.M.; Papineau, D.; Bleeker, W.; Downs, R.T.; Ferry, F.; McCoy, T.; Sverjensky, D.; Yang, H.: Mineral evolution, American Mineralogist 93 (2008) 1693–1720 DOI: 10.2138/am.2008.295510.2138/am.2008.2955Search in Google Scholar

Received: 2021-06-07
Accepted: 2021-07-23
Published Online: 2021-09-11
Published in Print: 2021-09-30

© 2021 Walter de Gruyter GmbH, Berlin/Boston, Germany

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