Abstract

Magnetic mapping is a common method for investigating archaeological sites. Typically, the magnetic field data are treated with basic signal improving processing followed by image interpretation to derive the location and outline of archaeological objects. However, the magnetic maps can yield more information; we present a two-step automatized interpretation scheme that enables us to infer the social structure from the magnetic map. First, we derive the magnetization distribution via inverse filtering by assuming a constant depth range for the building remains. Second, we quantify the building remains in terms of their total magnetic moment. In our field example, we consider this quantity as a proxy of household prosperity and its distribution as a social indicator. The inverse filtering approach is tested on synthetic data and cross-checked with a least-squares inversion. An extensive modeling study highlights the influence of depth and thickness of the layer for the filter construction. We deduce the rule of thumb that by choosing a rather too deep and too thick a layer, errors are smaller than for layers too low and too thin. The interpretation scheme is applied to the magnetic gradiometry map of the Chalcolithic Cucuteni–Tripolye site Maidanetske (Ukraine) that comprises the anomalies of about 2300 burned clay buildings. The buildings are arranged along concentric ellipses around an inner vacant space and a vacant ring. Buildings along this ring corridor have increased total magnetic moments. The total magnetic moment indicates the remaining building material and therefore the architecture. Lastly, architecture can reflect economic or social status. Consequently, the increased magnetic moment of buildings along the ring corridor indicates a higher economic or social status. The example of Maidanetske provides convincing evidence that the inversion of magnetic data and the quantification of buildings in terms of their magnetic moments enables the investigation of the social structure within sites.

Highlights

  • Magnetic gradiometry is commonly performed in archaeological projects to map the layout of sites

  • The interpretation scheme consists of two parts presented : (1) the derivation of the magnetization distribution by inverse filtering and (2) the quantification of the buildings using the magnetization distribution

  • To infer the social structure of archaeological sites, we presented an interpretation scheme based on magnetic prospection data

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Summary

Introduction

Magnetic gradiometry is commonly performed in archaeological projects to map the layout of sites. Inversion calculations to determine the three-dimensional geometry or the magnetization are rarely performed. The seldom inversion of magnetic data originates from the inherent ambiguity of potential field data and the lack of constraints. The ambiguity and the need for constraints lead to specific inversion schemes for individual sites (e.g., [3,4,5,6,7,8,9,10]). The inversion computations are applied to selected magnetic anomalies rather than to complete sites. Applying an inversion scheme to a complete site leads to a new quality of data that may contain information on the social structure of the bygone inhabitants

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