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An integrated magnetic, geochemical and archeointensity investigation of casting debris from ancient metallurgical sites of Michoacán, Western Mesoamerica

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Abstract

The ability of baked clay-elaborated objects to record the temporal variations of both direction and intensity of the geomagnetic field at the time of their elaboration or last use has been widely used during the last decades to fill the gaps left by available time-discrete volcanic-rock logs for a better knowledge of the evolution of the geomagnetic field. Further refinement of the secular variation curves has motivated the search for alternative non-conventional materials as attractive targets for archeomagnetic studies. Both clay and copper have been used since pre-Hispanic times for the elaboration of a wide variety of ornamental and utilitarian objects in Mesoamerica. Previous studies carried out in Europe and Israel have shown the usefulness of copper slags as one of these non-conventional materials. We present the results of an integrated study carried out on ten copper slags from seven ancient metallurgical sites of Michoacán. The analysis included a series of rock magnetism experiments, scanning electron microscope analysis, archeointensity determinations following the Thellier-Coe method and their corresponding dating. Based on the results obtained the slag-set analyzed can be divided in two main groups: low Fe concentrations (associated with high Cu concentrations) for slags comprising the first group, and high Fe concentrations (associated with low Cu concentrations) for slags from second group. Slags from the first group are characterized by almost reversible thermomagnetic curves, while those corresponding to the second group show a quite irreversible behavior. A crystalline (vitreous) structure within the massive surface of the slags is observed for those coming from the second (first) group. These striking features could reflect significant differences in the metallurgical process followed at these sites, which according to archeological and historical evidences correspond to Colonial and pre-Hispanic usage metallurgical sites; first and second group, respectively. The good experimental behavior exhibited by these materials demonstrates the suitability of copper slag to obtaining absolute archeointensity data which can be used to improve the existing Mesoamerican archeomagnetic record. This in turn, can be used both for geomagnetic field modelling purposes and archeomagnetic dating.

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Authors and Affiliations

  1. Laboratorio Interinstitucional de Magnetismo Natural, Instituto de Geofísica, Unidad Michoacán, Universidad Nacional Autonoma de México, Campus Morelia, 58190, Morelia, México

    Juan Morales & Avto Goguitchaichvili

  2. Servicio Arqueomagnético Nacional, Instituto de Geofísica, Unidad Michoacán, Universidad Nacional Autonoma de México, Campus Morelia, 58190, Morelia, México

    Juan Morales & Avto Goguitchaichvili

  3. Escuela Nacional de Estudios Superiores (ENES), Unidad Morelia, Universidad Nacional Autonoma de México, Campus Morelia, 58190, Morelia, México

    María del Sol Hernández-Bernal

  4. Instituto Nacional de Antropologia e Historia, Delegacion Michoacan, Madero Oriente 799, Morelia, México

    José Luis Punzo-Díaz

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  1. Juan Morales
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  2. María del Sol Hernández-Bernal
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  3. Avto Goguitchaichvili
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  4. José Luis Punzo-Díaz
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Correspondence to Juan Morales.

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Morales, J., del Sol Hernández-Bernal, M., Goguitchaichvili, A. et al. An integrated magnetic, geochemical and archeointensity investigation of casting debris from ancient metallurgical sites of Michoacán, Western Mesoamerica. Stud Geophys Geod 61, 290–309 (2017). https://doi.org/10.1007/s11200-016-1033-z

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  • DOI: https://doi.org/10.1007/s11200-016-1033-z

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